Articles | Volume 21, issue 8
https://doi.org/10.5194/nhess-21-2643-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/nhess-21-2643-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Review article
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01 Sep 2021
Review article | Highlight paper |
| 01 Sep 2021
| 01 Sep 2021
Sea-level rise in Venice: historic and future trends (review article)
Department of Environmental Sciences, Informatics and Statistics, University Ca’ Foscari of Venice, Via Torino 155, 30172 Mestre, Italy
Sara Bruni
Department of Physics and Astronomy, University of Bologna, Viale Berti Pichat 8, 40127 Bologna, Italy
now at: PosiTim UG, Seeheim-Jugenheim, Germany
Fabio Raicich
ISMAR – Marine Sciences Institute, CNR – National Research Council of Italy, AREA Science Park Q2 bldg, SS14 km 163.5, Basovizza, 34149 Trieste, Italy
Piero Lionello
Deptartment of Biological and Environmental Sciences and Technologies, Unversità del Salento, Centro Ecotekne Pal. M – S.P. 6, Lecce Monteroni, Italy
Fanny Adloff
National Centre for Atmospheric Science, University of Reading, Reading, UK
Alexey Androsov
Helmholtz Centre for Polar and Marine Research, Alfred Wegener Institute, Postfach 12-01-61, 27515, Bremerhaven, Germany
The St. Petersburg Department of the P.P. Shirshov Institute of Oceanology, RAS, 30, Pervaya Liniya, 199053, St. Petersburg, Russia
Fabrizio Antonioli
Istituto Nazionale di Geofisica e Vulcanologia, via di Vigna Murata 605, 00143 Rome, Italy
Vincenzo Artale
ENEA C.R. Frascati, SSPT-MET, Via Enrico Fermi 45, 00044 Frascati, Italy
Eugenio Carminati
Department of Earth Sciences, University of Rome La Sapienza, Piazzale Aldo Moro 5, 00185 Rome, Italy
Christian Ferrarin
ISMAR – Marine Sciences Institute, CNR – National Research Council of Italy, Castello 2737/F, 30122 Venice, Italy
Vera Fofonova
Helmholtz Centre for Polar and Marine Research, Alfred Wegener Institute, Postfach 12-01-61, 27515, Bremerhaven, Germany
Robert J. Nicholls
Tyndall Centre for Climate Change Research, University of East Anglia, Norwich NR4 7TJ, United Kingdom
Sara Rubinetti
Department of Environmental Sciences, Informatics and Statistics, University Ca’ Foscari of Venice, Via Torino 155, 30172 Mestre, Italy
Angelo Rubino
Department of Environmental Sciences, Informatics and Statistics, University Ca’ Foscari of Venice, Via Torino 155, 30172 Mestre, Italy
Gianmaria Sannino
ENEA Casaccia, Climate and Impact Modeling Lab, SSPT-MET-CLIM, Via Anguillarese 301, 00123 Rome, Italy
Giorgio Spada
Department of Physics and Astronomy, University of Bologna, Viale Berti Pichat 8, 40127 Bologna, Italy
Rémi Thiéblemont
Bureau de Recherches Géologiques et Minières “BRGM”, French Geological Survey, 3 Avenue, Claude Guillemin, CEDEX, 45060 Orléans, France
Michael Tsimplis
School of Law, City University of Hong Kong, Tat Chee Avenue, Kowloon, Hong Kong
Georg Umgiesser
ISMAR – Marine Sciences Institute, CNR – National Research Council of Italy, Castello 2737/F, 30122 Venice, Italy
Marine Research Institute, Klaipeda University, Klaipeda, Lithuania
Stefano Vignudelli
Institute of Biophysics, CNR, AREA Ricerca, Via Moruzzi 1, 56127 Pisa, Italy
Guy Wöppelmann
LIENSs, CNRS–La Rochelle University, 2 rue Olympe de Gouges, 17000 La Rochelle, France
Susanna Zerbini
Department of Physics and Astronomy, University of Bologna, Viale Berti Pichat 8, 40127 Bologna, Italy
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Matteo Mastropierro, Daniele Peano, and Davide Zanchettin
EGUsphere, https://doi.org/10.5194/egusphere-2024-823, https://doi.org/10.5194/egusphere-2024-823, 2024
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Md Jamal Uddin Khan, Inge Van Den Beld, Guy Wöppelmann, Laurent Testut, Alexa Latapy, and Nicolas Pouvreau
Earth Syst. Sci. Data, 15, 5739–5753, https://doi.org/10.5194/essd-15-5739-2023, https://doi.org/10.5194/essd-15-5739-2023, 2023
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Roderik S. W. van de Wal, Angélique Melet, Debora Bellafiore, Michalis Vousdoukas, Paula Camus, Christian Ferrarin, Gualbert Oude Essink, Ivan D. Haigh, Piero Lionello, Arjen Luijendijk, Alexandra Toimil, and Joanna Staneva
State Planet Discuss., https://doi.org/10.5194/sp-2023-38, https://doi.org/10.5194/sp-2023-38, 2023
Revised manuscript accepted for SP
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Sea level rise has major impacts in Europe which vary from place to place and in time depending on the source of the impacts. Flooding, erosion and saltwater intrusion lead via different pathways to various consequences in coastal regions across Europe. It causes damage to assets, environment and people for all three categories of impacts discussed in this paper. The paper provides an overview of the various impacts in Europe.
Angélique Melet, Roderik van de Wal, Angel Amores, Arne Arns, Alisée A. Chaigneau, Irina Dinu, Ivan D. Haigh, Tim H. J. Hermans, Piero Lionello, Marta Marcos, H. E. Markus Meier, Benoit Meyssignac, Matthew D. Palmer, Ronja Reese, Matthew J. R. Simpson, and Aimée Slangen
State Planet Discuss., https://doi.org/10.5194/sp-2023-36, https://doi.org/10.5194/sp-2023-36, 2023
Revised manuscript accepted for SP
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Luca Arpaia, Christian Ferrarin, Marco Bajo, and Georg Umgiesser
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Michele Livani, Lorenzo Petracchini, Christoforos Benetatos, Francesco Marzano, Andrea Billi, Eugenio Carminati, Carlo Doglioni, Patrizio Petricca, Roberta Maffucci, Giulia Codegone, Vera Rocca, Francesca Verga, and Ilaria Antoncecchi
Earth Syst. Sci. Data, 15, 4261–4293, https://doi.org/10.5194/essd-15-4261-2023, https://doi.org/10.5194/essd-15-4261-2023, 2023
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This paper presents subsurface geological and geophysical data from the Po Plain and the northern Adriatic Sea (north Italy). We collected and digitized data from 160 deep wells (including geophysical logs), 61 geological cross-sections, and 10 isobath maps. Furthermore, after a data accuracy analysis, we generated a simplified 3D geological model with several gridded surfaces separating units with different lithological properties. All data are available in delimited text files in ASCII format.
Andrea Storto, Yassmin Hesham Essa, Vincenzo de Toma, Alessandro Anav, Gianmaria Sannino, Rosalia Santoleri, and Chunxue Yang
Geosci. Model Dev., 16, 4811–4833, https://doi.org/10.5194/gmd-16-4811-2023, https://doi.org/10.5194/gmd-16-4811-2023, 2023
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Weather Clim. Dynam., 4, 639–661, https://doi.org/10.5194/wcd-4-639-2023, https://doi.org/10.5194/wcd-4-639-2023, 2023
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Melissa Wood, Ivan D. Haigh, Quan Quan Le, Hung Nghia Nguyen, Hoang Ba Tran, Stephen E. Darby, Robert Marsh, Nikolaos Skliris, Joël J.-M. Hirschi, Robert J. Nicholls, and Nadia Bloemendaal
Nat. Hazards Earth Syst. Sci., 23, 2475–2504, https://doi.org/10.5194/nhess-23-2475-2023, https://doi.org/10.5194/nhess-23-2475-2023, 2023
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We used a novel database of simulated tropical cyclone tracks to explore whether typhoon-induced storm surges present a future flood risk to low-lying coastal communities around the South China Sea. We found that future climate change is likely to change tropical cyclone behaviour to an extent that this increases the severity and frequency of storm surges to Vietnam, southern China, and Thailand. Consequently, coastal flood defences need to be reviewed for resilience against this future hazard.
Rasa Idzelytė, Natalja Čerkasova, Jovita Mėžinė, Toma Dabulevičienė, Artūras Razinkovas-Baziukas, Ali Ertürk, and Georg Umgiesser
Ocean Sci., 19, 1047–1066, https://doi.org/10.5194/os-19-1047-2023, https://doi.org/10.5194/os-19-1047-2023, 2023
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This work is focused on the impacts of climate change on a complex water flow system in the southeastern (SE) Baltic Sea, covering the Nemunas river basin and Curonian Lagoon. The results show that lagoon and sea will receive more water coming from the Nemunas. This will lead to a decreased frequency of saltwater inflow to the lagoon, and water will take less time to renew. Water temperatures in the entire lagoon and the SE Baltic Sea will increase steadily, and salinity values will decrease.
Roberto Ingrosso, Piero Lionello, Mario Marcello Miglietta, and Gianfausto Salvadori
Nat. Hazards Earth Syst. Sci., 23, 2443–2448, https://doi.org/10.5194/nhess-23-2443-2023, https://doi.org/10.5194/nhess-23-2443-2023, 2023
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Tornadoes represent disruptive and dangerous weather events. The prediction of these small-scale phenomena depends on the resolution of present weather forecast and climatic projections. This work discusses the occurrence of tornadoes in terms of atmospheric variables and provides analytical expressions for their conditional probability. These formulas represent a tool for tornado alert systems and for estimating the future evolution of tornado frequency and intensity in climate projections.
Christian Ferrarin, Florian Pantillon, Silvio Davolio, Marco Bajo, Mario Marcello Miglietta, Elenio Avolio, Diego S. Carrió, Ioannis Pytharoulis, Claudio Sanchez, Platon Patlakas, Juan Jesús González-Alemán, and Emmanouil Flaounas
Nat. Hazards Earth Syst. Sci., 23, 2273–2287, https://doi.org/10.5194/nhess-23-2273-2023, https://doi.org/10.5194/nhess-23-2273-2023, 2023
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The combined use of meteorological and ocean models enabled the analysis of extreme sea conditions driven by Medicane Ianos, which hit the western coast of Greece on 18 September 2020, flooding and damaging the coast. The large spread associated with the ensemble highlighted the high model uncertainty in simulating such an extreme weather event. The different simulations have been used for outlining hazard scenarios that represent a fundamental component of the coastal risk assessment.
Marco Bajo, Christian Ferrarin, Georg Umgiesser, Andrea Bonometto, and Elisa Coraci
Ocean Sci., 19, 559–579, https://doi.org/10.5194/os-19-559-2023, https://doi.org/10.5194/os-19-559-2023, 2023
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This work uses a hydrodynamic model which assimilates in situ data to reproduce tides, surges, and seiches in the Mediterranean basin. Furthermore, we study the periods of the barotropic modes of the Mediterranean and Adriatic basins. This research aims to improve the forecasting and reanalysis for operational warning and climatological studies. It aims also to reach a better knowledge of these sea level components in this area.
Manuel Aghito, Loris Calgaro, Knut-Frode Dagestad, Christian Ferrarin, Antonio Marcomini, Øyvind Breivik, and Lars Robert Hole
Geosci. Model Dev., 16, 2477–2494, https://doi.org/10.5194/gmd-16-2477-2023, https://doi.org/10.5194/gmd-16-2477-2023, 2023
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The newly developed ChemicalDrift model can simulate the transport and fate of chemicals in the ocean and in coastal regions. The model combines ocean physics, including transport due to currents, turbulence due to surface winds and the sinking of particles to the sea floor, with ocean chemistry, such as the partitioning, the degradation and the evaporation of chemicals. The model will be utilized for risk assessment of ocean and sea-floor contamination from pollutants emitted from shipping.
Fabio Raicich
Earth Syst. Sci. Data, 15, 1749–1763, https://doi.org/10.5194/essd-15-1749-2023, https://doi.org/10.5194/essd-15-1749-2023, 2023
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In the changing climate, long sea level time series are essential for studying the variability of the mean sea level and the occurrence of extreme events on different timescales. This work summarizes the rescue and quality control of the ultra-centennial sea level data set of Trieste, Italy. The whole time series is characterized by a linear trend of about 1.4 mm yr−1, the period corresponding to the altimetry coverage by a trend of about 3.0 mm yr−1, similarly to the global ocean.
Médéric Gravelle, Guy Wöppelmann, Kevin Gobron, Zuheir Altamimi, Mikaël Guichard, Thomas Herring, and Paul Rebischung
Earth Syst. Sci. Data, 15, 497–509, https://doi.org/10.5194/essd-15-497-2023, https://doi.org/10.5194/essd-15-497-2023, 2023
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We produced a reanalysis of GNSS data near tide gauges worldwide within the International GNSS Service. It implements advances in data modelling and corrections, extending the record length by about 7 years. A 28 % reduction in station velocity uncertainties is achieved over the previous solution. These estimates of vertical land motion at the coast supplement data from satellite altimetry or tide gauges for an improved understanding of sea level changes and their impacts along coastal areas.
Jeremy Rohmer, Remi Thieblemont, Goneri Le Cozannet, Heiko Goelzer, and Gael Durand
The Cryosphere, 16, 4637–4657, https://doi.org/10.5194/tc-16-4637-2022, https://doi.org/10.5194/tc-16-4637-2022, 2022
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To improve the interpretability of process-based projections of the sea-level contribution from land ice components, we apply the machine-learning-based
SHapley Additive exPlanationsapproach to a subset of a multi-model ensemble study for the Greenland ice sheet. This allows us to quantify the influence of particular modelling decisions (related to numerical implementation, initial conditions, or parametrisation of ice-sheet processes) directly in terms of sea-level change contribution.
Jeremy Rohmer, Deborah Idier, Remi Thieblemont, Goneri Le Cozannet, and François Bachoc
Nat. Hazards Earth Syst. Sci., 22, 3167–3182, https://doi.org/10.5194/nhess-22-3167-2022, https://doi.org/10.5194/nhess-22-3167-2022, 2022
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We quantify the influence of wave–wind characteristics, offshore water level and sea level rise (projected up to 2200) on the occurrence of flooding events at Gâvres, French Atlantic coast. Our results outline the overwhelming influence of sea level rise over time compared to the others. By showing the robustness of our conclusions to the errors in the estimation procedure, our approach proves to be valuable for exploring and characterizing uncertainties in assessments of future flooding.
Julius Schlumberger, Christian Ferrarin, Sebastiaan N. Jonkman, Manuel Andres Diaz Loaiza, Alessandro Antonini, and Sandra Fatorić
Nat. Hazards Earth Syst. Sci., 22, 2381–2400, https://doi.org/10.5194/nhess-22-2381-2022, https://doi.org/10.5194/nhess-22-2381-2022, 2022
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Flooding has serious impacts on the old town of Venice. This paper presents a framework combining a flood model with a flood-impact model to support improving protection against future floods in Venice despite the recently built MOSE barrier. Applying the framework to seven plausible flood scenarios, it was found that individual protection has a significant damage-mediating effect if the MOSE barrier does not operate as anticipated. Contingency planning thus remains important in Venice.
Begoña Pérez Gómez, Ivica Vilibić, Jadranka Šepić, Iva Međugorac, Matjaž Ličer, Laurent Testut, Claire Fraboul, Marta Marcos, Hassen Abdellaoui, Enrique Álvarez Fanjul, Darko Barbalić, Benjamín Casas, Antonio Castaño-Tierno, Srđan Čupić, Aldo Drago, María Angeles Fraile, Daniele A. Galliano, Adam Gauci, Branislav Gloginja, Víctor Martín Guijarro, Maja Jeromel, Marcos Larrad Revuelto, Ayah Lazar, Ibrahim Haktan Keskin, Igor Medvedev, Abdelkader Menassri, Mohamed Aïssa Meslem, Hrvoje Mihanović, Sara Morucci, Dragos Niculescu, José Manuel Quijano de Benito, Josep Pascual, Atanas Palazov, Marco Picone, Fabio Raicich, Mohamed Said, Jordi Salat, Erdinc Sezen, Mehmet Simav, Georgios Sylaios, Elena Tel, Joaquín Tintoré, Klodian Zaimi, and George Zodiatis
Ocean Sci., 18, 997–1053, https://doi.org/10.5194/os-18-997-2022, https://doi.org/10.5194/os-18-997-2022, 2022
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This description and mapping of coastal sea level monitoring networks in the Mediterranean and Black seas reveals the existence of 240 presently operational tide gauges. Information is provided about the type of sensor, time sampling, data availability, and ancillary measurements. An assessment of the fit-for-purpose status of the network is also included, along with recommendations to mitigate existing bottlenecks and improve the network, in a context of sea level rise and increasing extremes.
Sam White, Eduardo Moreno-Chamarro, Davide Zanchettin, Heli Huhtamaa, Dagomar Degroot, Markus Stoffel, and Christophe Corona
Clim. Past, 18, 739–757, https://doi.org/10.5194/cp-18-739-2022, https://doi.org/10.5194/cp-18-739-2022, 2022
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This study examines whether the 1600 Huaynaputina volcano eruption triggered persistent cooling in the North Atlantic. It compares previous paleoclimate simulations with new climate reconstructions from natural proxies and historical documents and finds that the reconstructions are consistent with, but do not support, an eruption trigger for persistent cooling. The study also analyzes societal impacts of climatic change in ca. 1600 and the use of historical observations in model–data comparison.
Davide Zanchettin, Claudia Timmreck, Myriam Khodri, Anja Schmidt, Matthew Toohey, Manabu Abe, Slimane Bekki, Jason Cole, Shih-Wei Fang, Wuhu Feng, Gabriele Hegerl, Ben Johnson, Nicolas Lebas, Allegra N. LeGrande, Graham W. Mann, Lauren Marshall, Landon Rieger, Alan Robock, Sara Rubinetti, Kostas Tsigaridis, and Helen Weierbach
Geosci. Model Dev., 15, 2265–2292, https://doi.org/10.5194/gmd-15-2265-2022, https://doi.org/10.5194/gmd-15-2265-2022, 2022
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This paper provides metadata and first analyses of the volc-pinatubo-full experiment of CMIP6-VolMIP. Results from six Earth system models reveal significant differences in radiative flux anomalies that trace back to different implementations of volcanic forcing. Surface responses are in contrast overall consistent across models, reflecting the large spread due to internal variability. A second phase of VolMIP shall consider both aspects toward improved protocol for volc-pinatubo-full.
Ioannis A. Daglis, Loren C. Chang, Sergio Dasso, Nat Gopalswamy, Olga V. Khabarova, Emilia Kilpua, Ramon Lopez, Daniel Marsh, Katja Matthes, Dibyendu Nandy, Annika Seppälä, Kazuo Shiokawa, Rémi Thiéblemont, and Qiugang Zong
Ann. Geophys., 39, 1013–1035, https://doi.org/10.5194/angeo-39-1013-2021, https://doi.org/10.5194/angeo-39-1013-2021, 2021
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We present a detailed account of the science programme PRESTO (PREdictability of the variable Solar–Terrestrial cOupling), covering the period 2020 to 2024. PRESTO was defined by a dedicated committee established by SCOSTEP (Scientific Committee on Solar-Terrestrial Physics). We review the current state of the art and discuss future studies required for the most effective development of solar–terrestrial physics.
Vera Fofonova, Tuomas Kärnä, Knut Klingbeil, Alexey Androsov, Ivan Kuznetsov, Dmitry Sidorenko, Sergey Danilov, Hans Burchard, and Karen Helen Wiltshire
Geosci. Model Dev., 14, 6945–6975, https://doi.org/10.5194/gmd-14-6945-2021, https://doi.org/10.5194/gmd-14-6945-2021, 2021
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We present a test case of river plume spreading to evaluate coastal ocean models. Our test case reveals the level of numerical mixing (due to parameterizations used and numerical treatment of processes in the model) and the ability of models to reproduce complex dynamics. The major result of our comparative study is that accuracy in reproducing the analytical solution depends less on the type of applied model architecture or numerical grid than it does on the type of advection scheme.
Piero Lionello, David Barriopedro, Christian Ferrarin, Robert J. Nicholls, Mirko Orlić, Fabio Raicich, Marco Reale, Georg Umgiesser, Michalis Vousdoukas, and Davide Zanchettin
Nat. Hazards Earth Syst. Sci., 21, 2705–2731, https://doi.org/10.5194/nhess-21-2705-2021, https://doi.org/10.5194/nhess-21-2705-2021, 2021
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In this review we describe the factors leading to the extreme water heights producing the floods of Venice. We discuss the different contributions, their relative importance, and the resulting compound events. We highlight the role of relative sea level rise and the observed past and very likely future increase in extreme water heights, showing that they might be up to 160 % higher at the end of the 21st century than presently.
Georg Umgiesser, Marco Bajo, Christian Ferrarin, Andrea Cucco, Piero Lionello, Davide Zanchettin, Alvise Papa, Alessandro Tosoni, Maurizio Ferla, Elisa Coraci, Sara Morucci, Franco Crosato, Andrea Bonometto, Andrea Valentini, Mirko Orlić, Ivan D. Haigh, Jacob Woge Nielsen, Xavier Bertin, André Bustorff Fortunato, Begoña Pérez Gómez, Enrique Alvarez Fanjul, Denis Paradis, Didier Jourdan, Audrey Pasquet, Baptiste Mourre, Joaquín Tintoré, and Robert J. Nicholls
Nat. Hazards Earth Syst. Sci., 21, 2679–2704, https://doi.org/10.5194/nhess-21-2679-2021, https://doi.org/10.5194/nhess-21-2679-2021, 2021
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The city of Venice relies crucially on a good storm surge forecast to protect its population and cultural heritage. In this paper, we provide a state-of-the-art review of storm surge forecasting, starting from examples in Europe and focusing on the Adriatic Sea and the Lagoon of Venice. We discuss the physics of storm surge, as well as the particular aspects of Venice and new techniques in storm surge modeling. We also give recommendations on what a future forecasting system should look like.
Piero Lionello, Robert J. Nicholls, Georg Umgiesser, and Davide Zanchettin
Nat. Hazards Earth Syst. Sci., 21, 2633–2641, https://doi.org/10.5194/nhess-21-2633-2021, https://doi.org/10.5194/nhess-21-2633-2021, 2021
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Venice is an iconic place, and a paradigm of huge historical and cultural value is at risk. The threat posed by floods has dramatically increased in recent decades and is expected to continue to grow – and even accelerate – through this century. There is a need to better understand the future evolution of the relative sea level and its extremes and to develop adaptive planning strategies appropriate for present uncertainty, which might not be substantially reduced in the near future.
Rémi Thiéblemont, Gonéri Le Cozannet, Jérémy Rohmer, Alexandra Toimil, Moisés Álvarez-Cuesta, and Iñigo J. Losada
Nat. Hazards Earth Syst. Sci., 21, 2257–2276, https://doi.org/10.5194/nhess-21-2257-2021, https://doi.org/10.5194/nhess-21-2257-2021, 2021
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Sea level rise and its acceleration are projected to aggravate coastal erosion over the 21st century. Resulting shoreline projections are deeply uncertain, however, which constitutes a major challenge for coastal planning and management. Our work presents a new extra-probabilistic framework to develop future shoreline projections and shows that deep uncertainties could be drastically reduced by better constraining sea level projections and improving coastal impact models.
Miroslav Gačić, Laura Ursella, Vedrana Kovačević, Milena Menna, Vlado Malačič, Manuel Bensi, Maria-Eletta Negretti, Vanessa Cardin, Mirko Orlić, Joël Sommeria, Ricardo Viana Barreto, Samuel Viboud, Thomas Valran, Boris Petelin, Giuseppe Siena, and Angelo Rubino
Ocean Sci., 17, 975–996, https://doi.org/10.5194/os-17-975-2021, https://doi.org/10.5194/os-17-975-2021, 2021
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Experiments in rotating tanks can simulate the Earth system and help to represent the real ocean, where rotation plays an important role. We wanted to show the minor importance of the wind in driving the flow in the Ionian Sea. We did this by observing changes in the water current in a rotating tank affected only by the pumping of dense water into the system. The flow variations were similar to those in the real sea, confirming the scarce importance of the wind for the flow in the Ionian Sea.
Claudia Timmreck, Matthew Toohey, Davide Zanchettin, Stefan Brönnimann, Elin Lundstad, and Rob Wilson
Clim. Past, 17, 1455–1482, https://doi.org/10.5194/cp-17-1455-2021, https://doi.org/10.5194/cp-17-1455-2021, 2021
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The 1809 eruption is one of the most recent unidentified volcanic eruptions with a global climate impact. We demonstrate that climate model simulations of the 1809 eruption show generally good agreement with many large-scale temperature reconstructions and early instrumental records for a range of radiative forcing estimates. In terms of explaining the spatially heterogeneous and temporally delayed Northern Hemisphere cooling suggested by tree-ring networks, the investigation remains open.
Fabio Raicich and Renato R. Colucci
Earth Syst. Sci. Data, 13, 3363–3377, https://doi.org/10.5194/essd-13-3363-2021, https://doi.org/10.5194/essd-13-3363-2021, 2021
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To understand climate change, it is essential to analyse long time series of atmospheric data. Here we studied the atmospheric pressure observed at Trieste (Italy) from 1841 to 2018. We examined the available information on the characteristics and elevations of the barometers and on the data sampling. A basic data quality control was also applied. As a result, we built a homogeneous time series of daily mean pressures at mean sea level, from which a trend of 0.5 hPa per century was estimated.
Paula Camus, Ivan D. Haigh, Ahmed A. Nasr, Thomas Wahl, Stephen E. Darby, and Robert J. Nicholls
Nat. Hazards Earth Syst. Sci., 21, 2021–2040, https://doi.org/10.5194/nhess-21-2021-2021, https://doi.org/10.5194/nhess-21-2021-2021, 2021
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In coastal regions, floods can arise through concurrent drivers, such as precipitation, river discharge, storm surge, and waves, which exacerbate the impact. In this study, we identify hotspots of compound flooding along the southern coast of the North Atlantic Ocean and the northern coast of the Mediterranean Sea. This regional assessment can be considered a screening tool for coastal management that provides information about which areas are more predisposed to experience compound flooding.
Alessandro Anav, Adriana Carillo, Massimiliano Palma, Maria Vittoria Struglia, Ufuk Utku Turuncoglu, and Gianmaria Sannino
Geosci. Model Dev., 14, 4159–4185, https://doi.org/10.5194/gmd-14-4159-2021, https://doi.org/10.5194/gmd-14-4159-2021, 2021
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The Mediterranean Basin is a complex region, characterized by the presence of pronounced topography and a complex land–sea distribution including a considerable number of islands and straits; these features generate strong local atmosphere–sea interactions.
Regional Earth system models have been developed and used to study both present and future Mediterranean climate systems. The main aims of this paper are to present and evaluate the newly developed regional Earth system model ENEA-REG.
Margot Clyne, Jean-Francois Lamarque, Michael J. Mills, Myriam Khodri, William Ball, Slimane Bekki, Sandip S. Dhomse, Nicolas Lebas, Graham Mann, Lauren Marshall, Ulrike Niemeier, Virginie Poulain, Alan Robock, Eugene Rozanov, Anja Schmidt, Andrea Stenke, Timofei Sukhodolov, Claudia Timmreck, Matthew Toohey, Fiona Tummon, Davide Zanchettin, Yunqian Zhu, and Owen B. Toon
Atmos. Chem. Phys., 21, 3317–3343, https://doi.org/10.5194/acp-21-3317-2021, https://doi.org/10.5194/acp-21-3317-2021, 2021
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This study finds how and why five state-of-the-art global climate models with interactive stratospheric aerosols differ when simulating the aftermath of large volcanic injections as part of the Model Intercomparison Project on the climatic response to Volcanic forcing (VolMIP). We identify and explain the consequences of significant disparities in the underlying physics and chemistry currently in some of the models, which are problems likely not unique to the models participating in this study.
Gonéri Le Cozannet, Déborah Idier, Marcello de Michele, Yoann Legendre, Manuel Moisan, Rodrigo Pedreros, Rémi Thiéblemont, Giorgio Spada, Daniel Raucoules, and Ywenn de la Torre
Nat. Hazards Earth Syst. Sci., 21, 703–722, https://doi.org/10.5194/nhess-21-703-2021, https://doi.org/10.5194/nhess-21-703-2021, 2021
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Chronic flooding occurring at high tides under calm weather conditions is an early impact of sea-level rise. This hazard is a reason for concern on tropical islands, where coastal infrastructure is commonly located in low-lying areas. We focus here on the Guadeloupe archipelago, in the French Antilles, where chronic flood events have been reported for about 10 years. We show that the number of such events will increase drastically over the 21st century under continued growth of CO2 emissions.
Christian Ferrarin, Marco Bajo, and Georg Umgiesser
Geosci. Model Dev., 14, 645–659, https://doi.org/10.5194/gmd-14-645-2021, https://doi.org/10.5194/gmd-14-645-2021, 2021
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The problem of the optimization of ocean monitoring networks is tackled through the implementation of data assimilation techniques in a numerical model. The methodology has been applied to the tide gauge network in the Lagoon of Venice (Italy). The data assimilation methods allow identifying the minimum number of stations and their distribution that correctly represent the lagoon's dynamics. The methodology is easily exportable to other environments and can be extended to other variables.
Lucia Pineau-Guillou, Pascal Lazure, and Guy Wöppelmann
Ocean Sci., 17, 17–34, https://doi.org/10.5194/os-17-17-2021, https://doi.org/10.5194/os-17-17-2021, 2021
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We investigated the long-term changes of the principal tidal component M2 along North Atlantic coasts, from 1846 to 2018. We analysed 18 tide gauges. We found that M2 variations are consistent at all the stations in the North-East Atlantic, whereas some discrepancies appear in the North-West Atlantic. The similarity between the North Atlantic Oscillation and M2 variations in the North-East Atlantic suggests a possible influence of the large-scale atmospheric circulation on the tide.
Fabio Raicich
Hist. Geo Space. Sci., 11, 1–14, https://doi.org/10.5194/hgss-11-1-2020, https://doi.org/10.5194/hgss-11-1-2020, 2020
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The ongoing sea level rise is a big concern in the context of present climatic change. The study of past sea level observations is of great importance in describing sea level variations. This work describes the rescue and analysis of a previously unrecognised 12-year record of sea level heights, measured at Trieste in the late 18th century. Besides having historical value, the data were found to be consistent, although undocumented technical issues limited the scientific conclusions.
Christian Ferrarin, Andrea Valentini, Martin Vodopivec, Dijana Klaric, Giovanni Massaro, Marco Bajo, Francesca De Pascalis, Amedeo Fadini, Michol Ghezzo, Stefano Menegon, Lidia Bressan, Silvia Unguendoli, Anja Fettich, Jure Jerman, Matjaz̆ Ličer, Lidija Fustar, Alvise Papa, and Enrico Carraro
Nat. Hazards Earth Syst. Sci., 20, 73–93, https://doi.org/10.5194/nhess-20-73-2020, https://doi.org/10.5194/nhess-20-73-2020, 2020
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Here we present a shared and interoperable system to allow a better exchange of and elaboration on information related to sea storms among countries. The proposed integrated web system (IWS) is a combination of a common data system for sharing ocean observations and forecasts, a multi-model ensemble system, a geoportal, and interactive geo-visualization tools. This study describes the application of the developed system to the exceptional storm event of 29 October 2018.
Vera Fofonova, Alexey Androsov, Lasse Sander, Ivan Kuznetsov, Felipe Amorim, H. Christian Hass, and Karen H. Wiltshire
Ocean Sci., 15, 1761–1782, https://doi.org/10.5194/os-15-1761-2019, https://doi.org/10.5194/os-15-1761-2019, 2019
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This study is dedicated to tidally induced dynamics in the Sylt-Rømø Bight with a focus on the non-linear component. The tidal residual circulation and asymmetric tidal cycles largely define the circulation pattern, transport and accumulation of sediment, and the distribution of bedforms. The newly obtained high-quality bathymetric data supported the use of high-resolution grids (up to 2 m in the intertidal zone) and elaboration of the details of tidal energy transformation in the domain.
Ivan Kuznetsov, Alexey Androsov, Vera Fofonova, Sergey Danilov, Natalja Rakowsky, Sven Harig, and Karen Helen Wiltshire
Ocean Sci. Discuss., https://doi.org/10.5194/os-2019-103, https://doi.org/10.5194/os-2019-103, 2019
Revised manuscript not accepted
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Coastal regions play a significant role in global processes. Numerical models are one of the major instruments in understanding ocean dynamics. The main objective of this article is to demonstrate the representativeness of the simulations with the new FESOM-C model by comparing the results with observational data for the southeastern part of the North Sea. An equally important objective is to present the application of convergence analysis of solutions for grids of different spatial resolutions.
Piero Lionello, Dario Conte, and Marco Reale
Nat. Hazards Earth Syst. Sci., 19, 1541–1564, https://doi.org/10.5194/nhess-19-1541-2019, https://doi.org/10.5194/nhess-19-1541-2019, 2019
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Large positive and negative sea level anomalies on the coast of the Mediterranean Sea are produced by cyclones moving along the Mediterranean storm track, which are mostly generated in the western Mediterranean. The wind around the cyclone center is the main cause of sea level anomalies when a shallow water fetch is present. The inverse barometer effect produces a positive anomaly near the cyclone pressure minimum and a negative anomaly at the opposite side of the Mediterranean Sea.
Alistair Hendry, Ivan D. Haigh, Robert J. Nicholls, Hugo Winter, Robert Neal, Thomas Wahl, Amélie Joly-Laugel, and Stephen E. Darby
Hydrol. Earth Syst. Sci., 23, 3117–3139, https://doi.org/10.5194/hess-23-3117-2019, https://doi.org/10.5194/hess-23-3117-2019, 2019
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Flooding can arise from multiple sources, including waves, extreme sea levels, rivers, and severe rainfall. When two or more sources combine, the consequences can be greatly multiplied. We find the potential for the joint occurrence of extreme sea levels and river discharge to be greater on the western coast of the UK compared to the eastern coast. This is due to the weather conditions generating each flood source around the UK. These results will help increase our flood forecasting ability.
Fabio Raicich and Renato R. Colucci
Earth Syst. Sci. Data, 11, 761–768, https://doi.org/10.5194/essd-11-761-2019, https://doi.org/10.5194/essd-11-761-2019, 2019
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Thanks to near-surface sea temperatures measured at Trieste, northern Adriatic Sea, from 1899 to 2015, we estimated mean daily temperatures at 2 m depth and built a quasi-homogeneous 117-year-long time series. We describe the instruments used and the sites of measurements, which are all within Trieste harbour. The data set represents a valuable tool to study sea temperature variability on different timescales. A mean temperature rise rate of 1.1 ± 0.3 °C per century was estimated.
Athanasios T. Vafeidis, Mark Schuerch, Claudia Wolff, Tom Spencer, Jan L. Merkens, Jochen Hinkel, Daniel Lincke, Sally Brown, and Robert J. Nicholls
Nat. Hazards Earth Syst. Sci., 19, 973–984, https://doi.org/10.5194/nhess-19-973-2019, https://doi.org/10.5194/nhess-19-973-2019, 2019
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This paper evaluates the effect of surge water level reduction due to land surface characteristics when assessing flood impacts at global scales. Our results show that uncertainties due to not accounting for water attenuation are of similar magnitude to the uncertainties regarding the total amount of sea-level rise expected by 2100, thus highlighting the need for better understanding of the spatial and temporal variation of water levels across floodplains.
Alexey Androsov, Vera Fofonova, Ivan Kuznetsov, Sergey Danilov, Natalja Rakowsky, Sven Harig, Holger Brix, and Karen Helen Wiltshire
Geosci. Model Dev., 12, 1009–1028, https://doi.org/10.5194/gmd-12-1009-2019, https://doi.org/10.5194/gmd-12-1009-2019, 2019
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We present a description of a coastal ocean circulation model designed to work on variable-resolution meshes made of triangular and quadrilateral cells. This hybrid mesh functionality allows for higher numerical performance and less dissipative solutions.
Sophie Bastin, Philippe Drobinski, Marjolaine Chiriaco, Olivier Bock, Romain Roehrig, Clemente Gallardo, Dario Conte, Marta Domínguez Alonso, Laurent Li, Piero Lionello, and Ana C. Parracho
Atmos. Chem. Phys., 19, 1471–1490, https://doi.org/10.5194/acp-19-1471-2019, https://doi.org/10.5194/acp-19-1471-2019, 2019
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This paper uses colocated observations of temperature, precipitation and humidity to investigate the triggering of precipitation. It shows that there is a critical value of humidity above which precipitation picks up. This critical value depends on T and varies spatially. It also analyses how this dependency is reproduced in regional climate simulations over Europe. Models with too little and too light precipitation have both lower critical value of humidity and higher probability to exceed it.
Ilaria Isola, Giovanni Zanchetta, Russell N. Drysdale, Eleonora Regattieri, Monica Bini, Petra Bajo, John C. Hellstrom, Ilaria Baneschi, Piero Lionello, Jon Woodhead, and Alan Greig
Clim. Past, 15, 135–151, https://doi.org/10.5194/cp-15-135-2019, https://doi.org/10.5194/cp-15-135-2019, 2019
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To understand the natural variability in the climate system, the hydrological aspect (dry and wet conditions) is particularly important for its impact on our societies. The reconstruction of past precipitation regimes can provide a useful tool for forecasting future climate changes. We use multi-proxy time series (oxygen and carbon isotopes, trace elements) from a speleothem to investigate circulation pattern variations and seasonality effects during the dry 4.2 ka event in central Italy.
Winfried Hoke, Tina Swierczynski, Peter Braesicke, Karin Lochte, Len Shaffrey, Martin Drews, Hilppa Gregow, Ralf Ludwig, Jan Even Øie Nilsen, Elisa Palazzi, Gianmaria Sannino, Lars Henrik Smedsrud, and ECRA network
Adv. Geosci., 46, 1–10, https://doi.org/10.5194/adgeo-46-1-2019, https://doi.org/10.5194/adgeo-46-1-2019, 2019
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The European Climate Research Alliance is a bottom-up association of European research institutions helping to facilitate the development of climate change research, combining the capacities of national research institutions and inducing closer ties between existing national research initiatives, projects and infrastructures. This article briefly introduces the network's structure and organisation, as well as project management issues and prospects.
Antonio Sanchez-Roman, Gabriel Jorda, Gianmaria Sannino, and Damia Gomis
Ocean Sci., 14, 1547–1566, https://doi.org/10.5194/os-14-1547-2018, https://doi.org/10.5194/os-14-1547-2018, 2018
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We explore the vertical transfers of heat, salt and mass between the inflowing and outflowing layers at the Strait of Gibraltar by using a 3-D model with very high spatial resolution that allows for a realistic representation of the exchange. Results show a significant transformation of the water mass properties along their path through the strait, mainly induced by the recirculation of water between layers, while mixing seems to have little influence on the heat and salt exchanged.
Lauren Marshall, Anja Schmidt, Matthew Toohey, Ken S. Carslaw, Graham W. Mann, Michael Sigl, Myriam Khodri, Claudia Timmreck, Davide Zanchettin, William T. Ball, Slimane Bekki, James S. A. Brooke, Sandip Dhomse, Colin Johnson, Jean-Francois Lamarque, Allegra N. LeGrande, Michael J. Mills, Ulrike Niemeier, James O. Pope, Virginie Poulain, Alan Robock, Eugene Rozanov, Andrea Stenke, Timofei Sukhodolov, Simone Tilmes, Kostas Tsigaridis, and Fiona Tummon
Atmos. Chem. Phys., 18, 2307–2328, https://doi.org/10.5194/acp-18-2307-2018, https://doi.org/10.5194/acp-18-2307-2018, 2018
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We use four global aerosol models to compare the simulated sulfate deposition from the 1815 Mt. Tambora eruption to ice core records. Inter-model volcanic sulfate deposition differs considerably. Volcanic sulfate deposited on polar ice sheets is used to estimate the atmospheric sulfate burden and subsequently radiative forcing of historic eruptions. Our results suggest that deriving such relationships from model simulations may be associated with greater uncertainties than previously thought.
PAGES Hydro2k Consortium
Clim. Past, 13, 1851–1900, https://doi.org/10.5194/cp-13-1851-2017, https://doi.org/10.5194/cp-13-1851-2017, 2017
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Water availability is fundamental to societies and ecosystems, but our understanding of variations in hydroclimate (including extreme events, flooding, and decadal periods of drought) is limited due to a paucity of modern instrumental observations. We review how proxy records of past climate and climate model simulations can be used in tandem to understand hydroclimate variability over the last 2000 years and how these tools can also inform risk assessments of future hydroclimatic extremes.
Johann H. Jungclaus, Edouard Bard, Mélanie Baroni, Pascale Braconnot, Jian Cao, Louise P. Chini, Tania Egorova, Michael Evans, J. Fidel González-Rouco, Hugues Goosse, George C. Hurtt, Fortunat Joos, Jed O. Kaplan, Myriam Khodri, Kees Klein Goldewijk, Natalie Krivova, Allegra N. LeGrande, Stephan J. Lorenz, Jürg Luterbacher, Wenmin Man, Amanda C. Maycock, Malte Meinshausen, Anders Moberg, Raimund Muscheler, Christoph Nehrbass-Ahles, Bette I. Otto-Bliesner, Steven J. Phipps, Julia Pongratz, Eugene Rozanov, Gavin A. Schmidt, Hauke Schmidt, Werner Schmutz, Andrew Schurer, Alexander I. Shapiro, Michael Sigl, Jason E. Smerdon, Sami K. Solanki, Claudia Timmreck, Matthew Toohey, Ilya G. Usoskin, Sebastian Wagner, Chi-Ju Wu, Kok Leng Yeo, Davide Zanchettin, Qiong Zhang, and Eduardo Zorita
Geosci. Model Dev., 10, 4005–4033, https://doi.org/10.5194/gmd-10-4005-2017, https://doi.org/10.5194/gmd-10-4005-2017, 2017
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Climate model simulations covering the last millennium provide context for the evolution of the modern climate and for the expected changes during the coming centuries. They can help identify plausible mechanisms underlying palaeoclimatic reconstructions. Here, we describe the forcing boundary conditions and the experimental protocol for simulations covering the pre-industrial millennium. We describe the PMIP4 past1000 simulations as contributions to CMIP6 and additional sensitivity experiments.
Athanasios T. Vafeidis, Mark Schuerch, Claudia Wolff, Tom Spencer, Jan L. Merkens, Jochen Hinkel, Daniel Lincke, Sally Brown, and Robert J. Nicholls
Nat. Hazards Earth Syst. Sci. Discuss., https://doi.org/10.5194/nhess-2017-199, https://doi.org/10.5194/nhess-2017-199, 2017
Manuscript not accepted for further review
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Global assessments of coastal flooding are based on the assumption that water propagation follows a
bathtubpattern across the floodplain. Using a global model we find that this assumption can lead to overestimation of impacts, with an uncertainty range that can be of equal magnitude to uncertainties related to future sea-level rise. Our results highlight the importance of improving the representation of the spatial/temporal variation of water levels across floodplains of different landcover.
Darren M. Lumbroso, Natalie R. Suckall, Robert J. Nicholls, and Kathleen D. White
Nat. Hazards Earth Syst. Sci., 17, 1357–1373, https://doi.org/10.5194/nhess-17-1357-2017, https://doi.org/10.5194/nhess-17-1357-2017, 2017
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Recent coastal floods in the USA have highlighted a lack of resilience in poor communities. By researching successes from Bangladesh and Cuba, this paper details how lessons from these countries can reduce the vulnerability of less well-off or isolated American citizens to future coastal storm surges. The relevance of the lessons learnt from Cuba and Bangladesh to the USA was assessed. Transferable lessons include the importance of volunteerism and education in developing a “culture of safety”.
Andrés Payo, David Favis-Mortlock, Mark Dickson, Jim W. Hall, Martin D. Hurst, Mike J. A. Walkden, Ian Townend, Matthew C. Ives, Robert J. Nicholls, and Michael A. Ellis
Geosci. Model Dev., 10, 2715–2740, https://doi.org/10.5194/gmd-10-2715-2017, https://doi.org/10.5194/gmd-10-2715-2017, 2017
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CoastalME is a generic modelling environment to simulate coastal landscape evolution on spatial scales of kms to tens of kms, over decadal to centennial timescales. The novelty is that it simulates coastal morphology evolution as a set of dynamically linked raster and geometrical objects. Geometrical objects are derived from the raster structure providing a library of coastal elements (e.g. shoreline) that are conventionally used for modelling coastal behaviour on the timescales of interest.
Gianpiero Cossarini, Stefano Querin, Cosimo Solidoro, Gianmaria Sannino, Paolo Lazzari, Valeria Di Biagio, and Giorgio Bolzon
Geosci. Model Dev., 10, 1423–1445, https://doi.org/10.5194/gmd-10-1423-2017, https://doi.org/10.5194/gmd-10-1423-2017, 2017
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The BFMCOUPLER (v1.0) is a coupling scheme that links the MITgcm and BFM models for ocean biogeochemistry simulations. The online coupling is based on an open-source code characterizd by a modular structure. Modularity preserves the potentials of the two models, allowing for a sustainable programming effort to handle future evolutions in the two codes. The BFMCOUPLER code is released along with an idealized problem (a cyclonic gyre in a mid-latitude closed basin).
Nadia Pinardi, Vladyslav Lyubartsev, Nicola Cardellicchio, Claudio Caporale, Stefania Ciliberti, Giovanni Coppini, Francesca De Pascalis, Lorenzo Dialti, Ivan Federico, Marco Filippone, Alessandro Grandi, Matteo Guideri, Rita Lecci, Lamberto Lamberti, Giuliano Lorenzetti, Paolo Lusiani, Cosimo Damiano Macripo, Francesco Maicu, Michele Mossa, Diego Tartarini, Francesco Trotta, Georg Umgiesser, and Luca Zaggia
Nat. Hazards Earth Syst. Sci., 16, 2623–2639, https://doi.org/10.5194/nhess-16-2623-2016, https://doi.org/10.5194/nhess-16-2623-2016, 2016
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A multiscale sampling experiment was carried out in the Gulf of Taranto (eastern Mediterranean) providing the first synoptic evidence of the large-scale circulation structure and associated mesoscale variability. The circulation is shown to be dominated by an anticyclonic gyre and upwelling areas at the gyre periphery.
Davide Zanchettin, Myriam Khodri, Claudia Timmreck, Matthew Toohey, Anja Schmidt, Edwin P. Gerber, Gabriele Hegerl, Alan Robock, Francesco S. R. Pausata, William T. Ball, Susanne E. Bauer, Slimane Bekki, Sandip S. Dhomse, Allegra N. LeGrande, Graham W. Mann, Lauren Marshall, Michael Mills, Marion Marchand, Ulrike Niemeier, Virginie Poulain, Eugene Rozanov, Angelo Rubino, Andrea Stenke, Kostas Tsigaridis, and Fiona Tummon
Geosci. Model Dev., 9, 2701–2719, https://doi.org/10.5194/gmd-9-2701-2016, https://doi.org/10.5194/gmd-9-2701-2016, 2016
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Simulating volcanically-forced climate variability is a challenging task for climate models. The Model Intercomparison Project on the climatic response to volcanic forcing (VolMIP) – an endorsed contribution to CMIP6 – defines a protocol for idealized volcanic-perturbation experiments to improve comparability of results across different climate models. This paper illustrates the design of VolMIP's experiments and describes the aerosol forcing input datasets to be used.
Vera Fofonova, Igor Zhilyaev, Marina Krayneva, Dina Yakshina, Nikita Tananaev, Nina Volkova, and Karen H. Wiltshire
Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2016-254, https://doi.org/10.5194/hess-2016-254, 2016
Manuscript not accepted for further review
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This paper analyses water temperature characteristics in the basin outlet area of the Lena River during the summer season. The analysis is based on a long-term data series at several gauging stations including rare used data, however, which are important for understanding processes in the considered area. We discuss to what extent the water temperature observations near river bank represent the mean stream temperature. As an instrument statistical and deterministic modelling approaches are used.
Sara Biolchi, Stefano Furlani, Fabrizio Antonioli, Niccoló Baldassini, Joanna Causon Deguara, Stefano Devoto, Agata Di Stefano, Julian Evans, Timothy Gambin, Ritienne Gauci, Giuseppe Mastronuzzi, Carmelo Monaco, and Giovanni Scicchitano
Nat. Hazards Earth Syst. Sci., 16, 737–756, https://doi.org/10.5194/nhess-16-737-2016, https://doi.org/10.5194/nhess-16-737-2016, 2016
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Along the eastern coast of Malta, the processes responsible for the transport of anomalous large boulders from the sea to the coast were analysed. The wave heights required to transport them from the sea to the coast were estimated using a hydrodynamic approach, while AMS 14C ages were determined from encrusted marine organisms. The combination of the results suggests that the majority of boulders were detached and moved by storm waves, but the occurrence of past tsunamis cannot be ruled out.
Georg Umgiesser, Petras Zemlys, Ali Erturk, Arturas Razinkova-Baziukas, Jovita Mėžinė, and Christian Ferrarin
Ocean Sci., 12, 391–402, https://doi.org/10.5194/os-12-391-2016, https://doi.org/10.5194/os-12-391-2016, 2016
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The paper explores the importance of physical forcing on the exchange mechanisms and the renewal time in the Curonian Lagoon over 10 years. The influence of ice cover on the exchange rates has been explored. Finally, the influence of water level fluctuations and river discharge has been studied. It has been found that ice cover is surprisingly not very important for changes in renewal time. The single most important factor is river discharge.
W. J. McKiver, G. Sannino, F. Braga, and D. Bellafiore
Ocean Sci., 12, 51–69, https://doi.org/10.5194/os-12-51-2016, https://doi.org/10.5194/os-12-51-2016, 2016
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First modeling work comparing SHYFEM and MITgcm performance in the north Adriatic Sea; the treatment of heat/mass fluxes at the surface affects the models skill to reproduce coastal processes; high resolution is needed close to the coast, while lower resolution in the offshore is adequate to capture the dense water event; correct river discharges and temperature are vital for the reproduction of estuarine dynamics; non-hydrostatic processes do not influence the dense water formation.
J. Armstrong, R. Wilby, and R. J. Nicholls
Nat. Hazards Earth Syst. Sci., 15, 2511–2524, https://doi.org/10.5194/nhess-15-2511-2015, https://doi.org/10.5194/nhess-15-2511-2015, 2015
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A criterion to categorise climate change adaptation frameworks is presented denoting characteristics of three key frameworks established in the literature: scenario–led, decision-centric and vulnerability–led. Applying the criterion, the usability of frameworks is examined in coastal Suffolk. Results indicate adaptation frameworks established in the literature are not utilised in isolation in everyday practice. In reality, hybrid approaches are utilised to overcome aspects of framework weakness.
A. J. Stevens, D. Clarke, R. J. Nicholls, and M. P. Wadey
Nat. Hazards Earth Syst. Sci., 15, 1215–1229, https://doi.org/10.5194/nhess-15-1215-2015, https://doi.org/10.5194/nhess-15-1215-2015, 2015
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Using census data, historic maps and hydrodynamic modelling, this paper presents a methodology for assessing how the exposure of people to flooding has changed over the last 200 years at the local level in the UK. The method is applied to two case studies at Portsea and Hayling Islands in the UK's Solent region. The analysis shows that for the case studies, population rise has, to date, had a much greater influence on exposure than sea level rise.
M. W. Strassburg, B. D. Hamlington, R. R. Leben, P. Manurung, J. Lumban Gaol, B. Nababan, S. Vignudelli, and K.-Y. Kim
Clim. Past, 11, 743–750, https://doi.org/10.5194/cp-11-743-2015, https://doi.org/10.5194/cp-11-743-2015, 2015
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The Southeast Asian sea regional sea level trends are some of the highest observed in the modern satellite altimeter record that now spans almost 2 decades. Here, we examine the 20-year trends in the region over the last 60 years using a sea level reconstruction, demonstrating that a significant portion of the trend variability in the region is related to natural climate variability, specifically to the Pacific Decadal Oscillation.
F. Raicich
Nat. Hazards Earth Syst. Sci., 15, 527–535, https://doi.org/10.5194/nhess-15-527-2015, https://doi.org/10.5194/nhess-15-527-2015, 2015
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Daily sea level data of the Venice Lagoon observed in the 18th century allow us to obtain a composite the time series of sea level anomalies relative to the mean sea level, spanning 1751--1769 and 1872--2004. From these data the frequency of remarkable storm surges is estimated. They appear to be more frequent in the second half of the 18th century than in the late 19th and 20th centuries. The historical flood on 4 November 1966 turns out to be the most severe during the entire period.
V. Cardin, G. Civitarese, D. Hainbucher, M. Bensi, and A. Rubino
Ocean Sci., 11, 53–66, https://doi.org/10.5194/os-11-53-2015, https://doi.org/10.5194/os-11-53-2015, 2015
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The results of this study reveal that the thermohaline properties in the study area in 2011 lie between the thermohaline characteristics of the EMT and those of the pre-EMT phase, indicating a possible slow return towards the latter. It highlights the relationship between the hydrological property distribution of the upper layer in the Levantine basin and the alternate circulation regimes in the Ionian, which modulates the salinity distribution in the Eastern Mediterranean Sea.
D. Hainbucher, A. Rubino, V. Cardin, T. Tanhua, K. Schroeder, and M. Bensi
Ocean Sci., 10, 669–682, https://doi.org/10.5194/os-10-669-2014, https://doi.org/10.5194/os-10-669-2014, 2014
P. Malanotte-Rizzoli, V. Artale, G. L. Borzelli-Eusebi, S. Brenner, A. Crise, M. Gacic, N. Kress, S. Marullo, M. Ribera d'Alcalà, S. Sofianos, T. Tanhua, A. Theocharis, M. Alvarez, Y. Ashkenazy, A. Bergamasco, V. Cardin, S. Carniel, G. Civitarese, F. D'Ortenzio, J. Font, E. Garcia-Ladona, J. M. Garcia-Lafuente, A. Gogou, M. Gregoire, D. Hainbucher, H. Kontoyannis, V. Kovacevic, E. Kraskapoulou, G. Kroskos, A. Incarbona, M. G. Mazzocchi, M. Orlic, E. Ozsoy, A. Pascual, P.-M. Poulain, W. Roether, A. Rubino, K. Schroeder, J. Siokou-Frangou, E. Souvermezoglou, M. Sprovieri, J. Tintoré, and G. Triantafyllou
Ocean Sci., 10, 281–322, https://doi.org/10.5194/os-10-281-2014, https://doi.org/10.5194/os-10-281-2014, 2014
O. Bothe, J. H. Jungclaus, and D. Zanchettin
Clim. Past, 9, 2471–2487, https://doi.org/10.5194/cp-9-2471-2013, https://doi.org/10.5194/cp-9-2471-2013, 2013
M. Reale and P. Lionello
Nat. Hazards Earth Syst. Sci., 13, 1707–1722, https://doi.org/10.5194/nhess-13-1707-2013, https://doi.org/10.5194/nhess-13-1707-2013, 2013
P. Zemlys, C. Ferrarin, G. Umgiesser, S. Gulbinskas, and D. Bellafiore
Ocean Sci., 9, 573–584, https://doi.org/10.5194/os-9-573-2013, https://doi.org/10.5194/os-9-573-2013, 2013
N. Rakowsky, A. Androsov, A. Fuchs, S. Harig, A. Immerz, S. Danilov, W. Hiller, and J. Schröter
Nat. Hazards Earth Syst. Sci., 13, 1629–1642, https://doi.org/10.5194/nhess-13-1629-2013, https://doi.org/10.5194/nhess-13-1629-2013, 2013
A. Sanna, P. Lionello, and S. Gualdi
Nat. Hazards Earth Syst. Sci., 13, 1567–1577, https://doi.org/10.5194/nhess-13-1567-2013, https://doi.org/10.5194/nhess-13-1567-2013, 2013
H. Mihanović, I. Vilibić, S. Carniel, M. Tudor, A. Russo, A. Bergamasco, N. Bubić, Z. Ljubešić, D. Viličić, A. Boldrin, V. Malačič, M. Celio, C. Comici, and F. Raicich
Ocean Sci., 9, 561–572, https://doi.org/10.5194/os-9-561-2013, https://doi.org/10.5194/os-9-561-2013, 2013
O. Bothe, J. H. Jungclaus, D. Zanchettin, and E. Zorita
Clim. Past, 9, 1089–1110, https://doi.org/10.5194/cp-9-1089-2013, https://doi.org/10.5194/cp-9-1089-2013, 2013
C. Ferrarin, M. Ghezzo, G. Umgiesser, D. Tagliapietra, E. Camatti, L. Zaggia, and A. Sarretta
Hydrol. Earth Syst. Sci., 17, 1733–1748, https://doi.org/10.5194/hess-17-1733-2013, https://doi.org/10.5194/hess-17-1733-2013, 2013
R. Mel, A. Sterl, and P. Lionello
Nat. Hazards Earth Syst. Sci., 13, 1135–1142, https://doi.org/10.5194/nhess-13-1135-2013, https://doi.org/10.5194/nhess-13-1135-2013, 2013
J. Segschneider, A. Beitsch, C. Timmreck, V. Brovkin, T. Ilyina, J. Jungclaus, S. J. Lorenz, K. D. Six, and D. Zanchettin
Biogeosciences, 10, 669–687, https://doi.org/10.5194/bg-10-669-2013, https://doi.org/10.5194/bg-10-669-2013, 2013
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Mithun Deb, James J. Benedict, Ning Sun, Zhaoqing Yang, Robert D. Hetland, David Judi, and Taiping Wang
Nat. Hazards Earth Syst. Sci., 24, 2461–2479, https://doi.org/10.5194/nhess-24-2461-2024, https://doi.org/10.5194/nhess-24-2461-2024, 2024
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We coupled earth system, hydrology, and hydrodynamic models to generate plausible and physically consistent ensembles of hurricane events and their associated water levels from the open coast to tidal rivers of Delaware Bay and River. Our results show that the hurricane landfall locations and the estuarine wind can significantly amplify the extreme surge in a shallow and converging system, especially when the wind direction aligns with the surge propagation direction.
Ming-Huei Chang, Yen-Chen Huang, Yu-Hsin Cheng, Chuen-Teyr Terng, Jinyi Chen, and Jyh Cherng Jan
Nat. Hazards Earth Syst. Sci., 24, 2481–2494, https://doi.org/10.5194/nhess-24-2481-2024, https://doi.org/10.5194/nhess-24-2481-2024, 2024
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Monitoring the long-term trends in sea surface warming is crucial for informed decision-making and adaptation. This study offers a comprehensive examination of prevalent trend extraction methods. We identify the least-squares regression as suitable for general tasks yet highlight the need to address seasonal signal-induced bias, i.e., the phase–distance imbalance. Our developed method, evaluated using simulated and real data, is unbiased and better than the conventional SST anomaly method.
Thomas P. Collings, Niall D. Quinn, Ivan D. Haigh, Joshua Green, Izzy Probyn, Hamish Wilkinson, Sanne Muis, William V. Sweet, and Paul D. Bates
Nat. Hazards Earth Syst. Sci., 24, 2403–2423, https://doi.org/10.5194/nhess-24-2403-2024, https://doi.org/10.5194/nhess-24-2403-2024, 2024
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Coastal areas are at risk of flooding from rising sea levels and extreme weather events. This study applies a new approach to estimating the likelihood of coastal flooding around the world. The method uses data from observations and computer models to create a detailed map of where these coastal floods might occur. The approach can predict flooding in areas for which there are few or no data available. The results can be used to help prepare for and prevent this type of flooding.
Guangsheng Zhao and Xiaojing Niu
Nat. Hazards Earth Syst. Sci., 24, 2303–2313, https://doi.org/10.5194/nhess-24-2303-2024, https://doi.org/10.5194/nhess-24-2303-2024, 2024
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The purpose of this study is to estimate the spatial distribution of the tsunami hazard in the South China Sea from the Manila subduction zone. The plate motion data are used to invert the degree of locking on the fault plane. The degree of locking is used to estimate the maximum possible magnitude of earthquakes and describe the slip distribution. A spatial distribution map of the 1000-year return period tsunami wave height in the South China Sea was obtained by tsunami hazard assessment.
Mandana Ghanavati, Ian R. Young, Ebru Kirezci, and Jin Liu
Nat. Hazards Earth Syst. Sci., 24, 2175–2190, https://doi.org/10.5194/nhess-24-2175-2024, https://doi.org/10.5194/nhess-24-2175-2024, 2024
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The paper examines the changes in shoreline position of the coast of south-east Australia over a 26-year period to determine whether changes are consistent with observed changes in ocean wave and storm surge climate. The results show that in regions where there have been significant changes in wave energy flux or wave direction, there have also been changes in shoreline position consistent with non-equilibrium longshore drift.
Ina Teutsch, Ralf Weisse, and Sander Wahls
Nat. Hazards Earth Syst. Sci., 24, 2065–2069, https://doi.org/10.5194/nhess-24-2065-2024, https://doi.org/10.5194/nhess-24-2065-2024, 2024
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We investigate buoy and radar measurement data from shallow depths in the southern North Sea. We analyze the role of solitons for the occurrence of rogue waves. This is done by computing the nonlinear soliton spectrum of each time series. In a previous study that considered a single measurement site, we found a connection between the shape of the soliton spectrum and the occurrence of rogue waves. In this study, results for two additional sites are reported.
Marc Igigabel, Marissa Yates, Michalis Vousdoukas, and Youssef Diab
Nat. Hazards Earth Syst. Sci., 24, 1951–1974, https://doi.org/10.5194/nhess-24-1951-2024, https://doi.org/10.5194/nhess-24-1951-2024, 2024
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Changes in sea levels alone do not determine the evolution of coastal hazards. Coastal hazard changes should be assessed using additional factors describing geomorphological configurations, metocean event types (storms, cyclones, long swells, and tsunamis), and the marine environment (e.g., coral reef state and sea ice extent). The assessment completed here, at regional scale including the coasts of mainland and overseas France, highlights significant differences in hazard changes.
Jani Särkkä, Jani Räihä, Mika Rantanen, and Matti Kämäräinen
Nat. Hazards Earth Syst. Sci., 24, 1835–1842, https://doi.org/10.5194/nhess-24-1835-2024, https://doi.org/10.5194/nhess-24-1835-2024, 2024
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We study the relationship between tracks of low-pressure systems and related sea level extremes. We perform the studies by introducing a method to simulate sea levels using synthetic low-pressure systems. We test the method using sites located along the Baltic Sea coast. We find high extremes, where the sea level extreme reaches up to 3.5 m. In addition, we add the maximal value of the mean level of the Baltic Sea (1 m), leading to a sea level of 4.5 m.
Alexey Androsov, Sven Harig, Natalia Zamora, Kim Knauer, and Natalja Rakowsky
Nat. Hazards Earth Syst. Sci., 24, 1635–1656, https://doi.org/10.5194/nhess-24-1635-2024, https://doi.org/10.5194/nhess-24-1635-2024, 2024
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Two numerical codes are used in a comparative analysis of the calculation of the tsunami wave due to an earthquake along the Peruvian coast. The comparison primarily evaluates the flow velocity fields in flooded areas. The relative importance of the various parts of the equations is determined, focusing on the nonlinear terms. The influence of the nonlinearity on the degree and volume of flooding, flow velocity, and small-scale fluctuations is determined.
Eric Mortensen, Timothy Tiggeloven, Toon Haer, Bas van Bemmel, Dewi Le Bars, Sanne Muis, Dirk Eilander, Frederiek Sperna Weiland, Arno Bouwman, Willem Ligtvoet, and Philip J. Ward
Nat. Hazards Earth Syst. Sci., 24, 1381–1400, https://doi.org/10.5194/nhess-24-1381-2024, https://doi.org/10.5194/nhess-24-1381-2024, 2024
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Current levels of coastal flood risk are projected to increase in coming decades due to various reasons, e.g. sea-level rise, land subsidence, and coastal urbanization: action is needed to minimize this future risk. We evaluate dykes and coastal levees, foreshore vegetation, zoning restrictions, and dry-proofing on a global scale to estimate what levels of risk reductions are possible. We demonstrate that there are several potential adaptation pathways forward for certain areas of the world.
Alice Abbate, José M. González Vida, Manuel J. Castro Díaz, Fabrizio Romano, Hafize Başak Bayraktar, Andrey Babeyko, and Stefano Lorito
Nat. Hazards Earth Syst. Sci. Discuss., https://doi.org/10.5194/nhess-2024-41, https://doi.org/10.5194/nhess-2024-41, 2024
Revised manuscript accepted for NHESS
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Modeling the tsunami generation due to a rapid submarine earthquake is a complex problem. We propose and test, under a variety of realistic conditions in a subduction zone, an efficient solution to this problem, and a tool which can compute the generation of any potential tsunami in any ocean of the world. We will explore in the future solutions which would allow us to model the tsunami generation also by slower (time-dependent) seafloor displacement.
Charlotte Lyddon, Nguyen Chien, Grigorios Vasilopoulos, Michael Ridgill, Sogol Moradian, Agnieszka Olbert, Thomas Coulthard, Andrew Barkwith, and Peter Robins
Nat. Hazards Earth Syst. Sci., 24, 973–997, https://doi.org/10.5194/nhess-24-973-2024, https://doi.org/10.5194/nhess-24-973-2024, 2024
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Recent storms in the UK, like Storm Ciara in 2020, show how vulnerable estuaries are to the combined effect of sea level and river discharge. We show the combinations of sea levels and river discharges that cause flooding in the Conwy estuary, N Wales. The results showed flooding was amplified under moderate conditions in the middle estuary and elsewhere sea state or river flow dominated the hazard. Combined sea and river thresholds can improve prediction and early warning of compound flooding.
Sergio Padilla, Íñigo Aniel-Quiroga, Rachid Omira, Mauricio González, Jihwan Kim, and Maria A. Baptista
EGUsphere, https://doi.org/10.5194/egusphere-2024-663, https://doi.org/10.5194/egusphere-2024-663, 2024
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The eruption of the Hunga Tonga-Hunga Ha’apai volcano in January 2022 triggered a global phenomenon, including an atmospheric wave and a volcano-meteorological tsunami (VMT). The tsunami, reaching as far as Callao, Peru, 10,000 km away, caused significant coastal impacts. A study delves into understanding these effects, particularly on vessel moorings safety. The findings underscore the importance of enhancing TWS and preparing port authorities for managing such rare events.
Shuaib Rasheed, Simon C. Warder, Yves Plancherel, and Matthew D. Piggott
Nat. Hazards Earth Syst. Sci., 24, 737–755, https://doi.org/10.5194/nhess-24-737-2024, https://doi.org/10.5194/nhess-24-737-2024, 2024
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Here we use a high-resolution bathymetry dataset of the Maldives archipelago, as well as corresponding high numerical model resolution, to carry out a scenario-based tsunami hazard assessment for the entire Maldives archipelago to investigate the potential impact of plausible far-field tsunamis across the Indian Ocean at the island scale. The results indicate that several factors contribute to mitigating and amplifying tsunami waves at the island scale.
Niels J. Korsgaard, Kristian Svennevig, Anne S. Søndergaard, Gregor Luetzenburg, Mimmi Oksman, and Nicolaj K. Larsen
Nat. Hazards Earth Syst. Sci., 24, 757–772, https://doi.org/10.5194/nhess-24-757-2024, https://doi.org/10.5194/nhess-24-757-2024, 2024
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A tsunami wave will leave evidence of erosion and deposition in coastal lakes, making it possible to determine the runup height and when it occurred. Here, we use four lakes now located at elevations of 19–91 m a.s.l. close to the settlement of Saqqaq, West Greenland, to show that at least two giant tsunamis occurred 7300–7600 years ago with runup heights larger than 40 m. We infer that any tsunamis from at least nine giga-scale landslides must have happened 8500–10 000 years ago.
Elke Magda Inge Meyer and Lidia Gaslikova
Nat. Hazards Earth Syst. Sci., 24, 481–499, https://doi.org/10.5194/nhess-24-481-2024, https://doi.org/10.5194/nhess-24-481-2024, 2024
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Storm tides for eight extreme historical storms in the German Bight are modelled using sets of slightly varying atmospheric conditions from the century reanalyses. Comparisons with the water level observations from the gauges Norderney, Cuxhaven and Husum show that single members of the reanalyses are suitable for the reconstruction of extreme storms. Storms with more northerly tracks show less variability within a set and have more potential for accurate reconstruction of extreme water levels.
Clare Lewis, Tim Smyth, Jess Neumann, and Hannah Cloke
Nat. Hazards Earth Syst. Sci., 24, 121–131, https://doi.org/10.5194/nhess-24-121-2024, https://doi.org/10.5194/nhess-24-121-2024, 2024
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Meteotsunami are the result of atmospheric disturbances and can impact coastlines causing injury, loss of life, and damage to assets. This paper introduces a novel intensity index to allow for the quantification of these events at the shoreline. This has the potential to assist in the field of natural hazard assessment. It was trialled in the UK but designed for global applicability and to become a widely accepted standard in coastal planning, meteotsunami forecasting, and early warning systems.
Chu-En Hsu, Katherine A. Serafin, Xiao Yu, Christie A. Hegermiller, John C. Warner, and Maitane Olabarrieta
Nat. Hazards Earth Syst. Sci., 23, 3895–3912, https://doi.org/10.5194/nhess-23-3895-2023, https://doi.org/10.5194/nhess-23-3895-2023, 2023
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Total water levels (TWLs) induced by tropical cyclones (TCs) are among the leading hazards faced by coastal communities. Using numerical models, we examined how TWL components (surge and wave runup) along the South Atlantic Bight varied during hurricanes Matthew (2016), Dorian (2019), and Isaias (2020). Peak surge and peak wave runup were dominated by wind speeds and relative positions to TCs. The exceedance time of TWLs was controlled by normalized distances to TC and TC translation speeds.
Jean Roger and Bernard Pelletier
Nat. Hazards Earth Syst. Sci. Discuss., https://doi.org/10.5194/nhess-2023-198, https://doi.org/10.5194/nhess-2023-198, 2023
Revised manuscript accepted for NHESS
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This study presents a catalogue of tsunamis having occurred in the Vanuatu Arc. It has been built based on the analysis of existing catalogues, historical documents, and sea-level data from the 5 coastal tide gauges. 100 tsunamis of local, regional or far-field origins are listed since 1863. 15 of them show maximum wave amplitude and/or run-up height of above 1 m and 8 between 0.3 and 1 m. Details are provided for particular events, including debated events or events with no known origin(s).
Maude Biguenet, Eric Chaumillon, Pierre Sabatier, Antoine Bastien, Emeline Geba, Fabien Arnaud, Thibault Coulombier, and Nathalie Feuillet
Nat. Hazards Earth Syst. Sci., 23, 3761–3788, https://doi.org/10.5194/nhess-23-3761-2023, https://doi.org/10.5194/nhess-23-3761-2023, 2023
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This work documents the impact of Hurricane Irma (2017) on the Codrington barrier and lagoon on Barbuda Island. Irma caused two wide breaches in the sandy barrier, which remained unopened for 250 years. The thick and extensive sand sheet at the top of the lagoon fill was attributed to Irma. This unique deposit in a 3700-year record confirms Irma's exceptional character. This case study illustrates the consequences of high-intensity hurricanes in low-lying islands in a global warming context.
Leigh Richard MacPherson, Arne Arns, Svenja Fischer, Fernando Javier Méndez, and Jürgen Jensen
Nat. Hazards Earth Syst. Sci., 23, 3685–3701, https://doi.org/10.5194/nhess-23-3685-2023, https://doi.org/10.5194/nhess-23-3685-2023, 2023
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Efficient adaptation planning for coastal flooding caused by extreme sea levels requires accurate assessments of the underlying hazard. Tide-gauge data alone are often insufficient for providing the desired accuracy but may be supplemented with historical information. We estimate extreme sea levels along the German Baltic coast and show that relying solely on tide-gauge data leads to underestimations. Incorporating historical information leads to improved estimates with reduced uncertainties.
Anne Margaret H. Smiley, Suzanne P. Thompson, Nathan S. Hall, and Michael F. Piehler
Nat. Hazards Earth Syst. Sci., 23, 3635–3649, https://doi.org/10.5194/nhess-23-3635-2023, https://doi.org/10.5194/nhess-23-3635-2023, 2023
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Floodwaters can deliver reactive nitrogen to sensitive aquatic systems and diminish water quality. We assessed the nitrogen removal capabilities of flooded habitats and urban landscapes. Differences in processing rates across land cover treatments and between nutrient treatments suggest that abundance and spatial distributions of habitats, as well as storm characteristics, influence landscape-scale nitrogen removal. Results have important implications for coastal development and climate change.
Marine Le Gal, Tomás Fernández-Montblanc, Enrico Duo, Juan Montes Perez, Paulo Cabrita, Paola Souto Ceccon, Véra Gastal, Paolo Ciavola, and Clara Armaroli
Nat. Hazards Earth Syst. Sci., 23, 3585–3602, https://doi.org/10.5194/nhess-23-3585-2023, https://doi.org/10.5194/nhess-23-3585-2023, 2023
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Assessing coastal hazards is crucial to mitigate flooding disasters. In this regard, coastal flood databases are valuable tools. This paper describes a new coastal flood map catalogue covering the entire European coastline, as well as the methodology to build it and its accuracy. The catalogue focuses on frequent extreme events and relies on synthetic scenarios estimated from local storm conditions. Flood-prone areas and regions sensitive to storm duration and water level peak were identified.
Neng-Ti Yu, Cheng-Hao Lu, I-Chin Yen, Jia-Hong Chen, Jiun-Yee Yen, and Shyh-Jeng Chyi
Nat. Hazards Earth Syst. Sci., 23, 3525–3542, https://doi.org/10.5194/nhess-23-3525-2023, https://doi.org/10.5194/nhess-23-3525-2023, 2023
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A paleotsunami deposit of cliff-top basalt debris was identified on the Penghu Islands in the southern Taiwan Strait and related to the 1661 earthquake in southwest Taiwan. A minimum wave height of 3.2 m is estimated to have rotated the biggest boulder for over 30 m landwards onto the cliff top at 2.5 m a.s.l. The event must have been huge compared to the 1994 M 6.4 earthquake with the ensuing 0.4 m high tsunami in the same area, validating the intimidating tsunami risks in the South China Sea.
Ye Yuan, Huaiwei Yang, Fujiang Yu, Yi Gao, Benxia Li, and Chuang Xing
Nat. Hazards Earth Syst. Sci., 23, 3487–3507, https://doi.org/10.5194/nhess-23-3487-2023, https://doi.org/10.5194/nhess-23-3487-2023, 2023
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Rip currents are narrow jets of offshore-directed flow that originated in the surf zone, which can take swimmers of all ability levels into deeper water unawares. In this study, a 1 m fine-resolution wave-resolving model was configured to study rip current variability and the optimal swimmer escape strategies. Multiple factors contribute to the survival of swimmers. However, for weak-to-moderate rip and longshore currents, swimming onshore consistently seems to be the most successful strategy.
Benedikt Mester, Thomas Vogt, Seth Bryant, Christian Otto, Katja Frieler, and Jacob Schewe
Nat. Hazards Earth Syst. Sci., 23, 3467–3485, https://doi.org/10.5194/nhess-23-3467-2023, https://doi.org/10.5194/nhess-23-3467-2023, 2023
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In 2019, Cyclone Idai displaced more than 478 000 people in Mozambique. In our study, we use coastal flood modeling and satellite imagery to construct a counterfactual cyclone event without the effects of climate change. We show that 12 600–14 900 displacements can be attributed to sea level rise and the intensification of storm wind speeds due to global warming. Our impact attribution study is the first one on human displacement and one of very few for a low-income country.
Olivier Cavalié, Frédéric Cappa, and Béatrice Pinel-Puysségur
Nat. Hazards Earth Syst. Sci., 23, 3235–3246, https://doi.org/10.5194/nhess-23-3235-2023, https://doi.org/10.5194/nhess-23-3235-2023, 2023
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Coastal areas are fragile ecosystems that face multiple hazards. In this study, we measured the downward motion of the Nice Côte d'Azur Airport (France) that was built on reclaimed area and found that it has subsided from 16 mm yr-1 in the 1990s to 8 mm yr-1 today. A continuous remote monitoring of the platform will provide key data for a detailed investigation of future subsidence maps, and this contribution will help to evaluate the potential failure of part of the airport platform.
Wagner L. L. Costa, Karin R. Bryan, and Giovanni Coco
Nat. Hazards Earth Syst. Sci., 23, 3125–3146, https://doi.org/10.5194/nhess-23-3125-2023, https://doi.org/10.5194/nhess-23-3125-2023, 2023
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For predicting flooding events at the coast, topo-bathymetric data are essential. However, elevation data can be unavailable. To tackle this issue, recent efforts have centred on the use of satellite-derived topography (SDT) and bathymetry (SDB). This work is aimed at evaluating their accuracy and use for flooding prediction in enclosed estuaries. Results show that the use of SDT and SDB in numerical modelling can produce similar predictions when compared to the surveyed elevation data.
Joshua Kiesel, Marvin Lorenz, Marcel König, Ulf Gräwe, and Athanasios T. Vafeidis
Nat. Hazards Earth Syst. Sci., 23, 2961–2985, https://doi.org/10.5194/nhess-23-2961-2023, https://doi.org/10.5194/nhess-23-2961-2023, 2023
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Among the Baltic Sea littoral states, Germany is anticipated to experience considerable damage as a result of increased coastal flooding due to sea-level rise (SLR). Here we apply a new modelling framework to simulate how flooding along the German Baltic Sea coast may change until 2100 if dikes are not upgraded. We find that the study region is highly exposed to flooding, and we emphasise the importance of current plans to update coastal protection in the future.
Zhang Haixia, Cheng Meng, and Fang Weihua
Nat. Hazards Earth Syst. Sci., 23, 2697–2717, https://doi.org/10.5194/nhess-23-2697-2023, https://doi.org/10.5194/nhess-23-2697-2023, 2023
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Simultaneous storm surge and waves can cause great damage due to cascading effects. Quantitative joint probability analysis is critical to determine their optimal protection design values. The joint probability of the surge and wave for the eastern coasts of Leizhou Peninsula and Hainan are estimated with a Gumbel copula based on 62 years of numerically simulated data, and the optimal design values under various joint return periods are derived using the non-linear programming method.
Clare Lewis, Tim Smyth, David Williams, Jess Neumann, and Hannah Cloke
Nat. Hazards Earth Syst. Sci., 23, 2531–2546, https://doi.org/10.5194/nhess-23-2531-2023, https://doi.org/10.5194/nhess-23-2531-2023, 2023
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Meteotsunami are globally occurring water waves initiated by atmospheric disturbances. Previous research has suggested that in the UK, meteotsunami are a rare phenomenon and tend to occur in the summer months. This article presents a revised and updated catalogue of 98 meteotsunami that occurred between 1750 and 2022. Results also demonstrate a larger percentage of winter events and a geographical pattern highlighting the
hotspotregions that experience these events.
Melissa Wood, Ivan D. Haigh, Quan Quan Le, Hung Nghia Nguyen, Hoang Ba Tran, Stephen E. Darby, Robert Marsh, Nikolaos Skliris, Joël J.-M. Hirschi, Robert J. Nicholls, and Nadia Bloemendaal
Nat. Hazards Earth Syst. Sci., 23, 2475–2504, https://doi.org/10.5194/nhess-23-2475-2023, https://doi.org/10.5194/nhess-23-2475-2023, 2023
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We used a novel database of simulated tropical cyclone tracks to explore whether typhoon-induced storm surges present a future flood risk to low-lying coastal communities around the South China Sea. We found that future climate change is likely to change tropical cyclone behaviour to an extent that this increases the severity and frequency of storm surges to Vietnam, southern China, and Thailand. Consequently, coastal flood defences need to be reviewed for resilience against this future hazard.
Sang-Guk Yum, Moon-Soo Song, and Manik Das Adhikari
Nat. Hazards Earth Syst. Sci., 23, 2449–2474, https://doi.org/10.5194/nhess-23-2449-2023, https://doi.org/10.5194/nhess-23-2449-2023, 2023
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This study performed analysis on typhoon-induced coastal morphodynamics for the Mokpo coast. Wetland vegetation was severely impacted by Typhoon Soulik, with 87.35 % of shoreline transects experiencing seaward migration. This result highlights the fact that sediment resuspension controls the land alteration process over the typhoon period. The land accretion process dominated during the pre- to post-typhoon periods.
Olle Räty, Marko Laine, Ulpu Leijala, Jani Särkkä, and Milla M. Johansson
Nat. Hazards Earth Syst. Sci., 23, 2403–2418, https://doi.org/10.5194/nhess-23-2403-2023, https://doi.org/10.5194/nhess-23-2403-2023, 2023
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We studied annual maximum sea levels in the Finnish coastal region. Our aim was to better quantify the uncertainty in them compared to previous studies. Using four statistical models, we found out that hierarchical models, which shared information on sea-level extremes across Finnish tide gauges, had lower uncertainty in their results in comparison with tide-gauge-specific fits. These models also suggested that the shape of the distribution for extreme sea levels is similar on the Finnish coast.
Christian Ferrarin, Florian Pantillon, Silvio Davolio, Marco Bajo, Mario Marcello Miglietta, Elenio Avolio, Diego S. Carrió, Ioannis Pytharoulis, Claudio Sanchez, Platon Patlakas, Juan Jesús González-Alemán, and Emmanouil Flaounas
Nat. Hazards Earth Syst. Sci., 23, 2273–2287, https://doi.org/10.5194/nhess-23-2273-2023, https://doi.org/10.5194/nhess-23-2273-2023, 2023
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The combined use of meteorological and ocean models enabled the analysis of extreme sea conditions driven by Medicane Ianos, which hit the western coast of Greece on 18 September 2020, flooding and damaging the coast. The large spread associated with the ensemble highlighted the high model uncertainty in simulating such an extreme weather event. The different simulations have been used for outlining hazard scenarios that represent a fundamental component of the coastal risk assessment.
Charline Dalinghaus, Giovanni Coco, and Pablo Higuera
Nat. Hazards Earth Syst. Sci., 23, 2157–2169, https://doi.org/10.5194/nhess-23-2157-2023, https://doi.org/10.5194/nhess-23-2157-2023, 2023
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Wave setup is a critical component of coastal flooding. Consequently, understanding and being able to predict wave setup is vital to protect coastal resources and the population living near the shore. Here, we applied machine learning to improve the accuracy of present predictors of wave setup. The results show that the new predictors outperform existing formulas demonstrating the capability of machine learning models to provide a physically sound description of wave setup.
Ina Teutsch, Markus Brühl, Ralf Weisse, and Sander Wahls
Nat. Hazards Earth Syst. Sci., 23, 2053–2073, https://doi.org/10.5194/nhess-23-2053-2023, https://doi.org/10.5194/nhess-23-2053-2023, 2023
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Rogue waves exceed twice the significant wave height. They occur more often than expected in the shallow waters off Norderney. When applying a nonlinear Fourier transform for the Korteweg–de Vries equation to wave data from Norderney, we found differences in the soliton spectra of time series with and without rogue waves. A strongly outstanding soliton in the spectrum indicated an enhanced probability for rogue waves. We could attribute spectral solitons to the measured rogue waves.
Philipp Heinrich, Stefan Hagemann, Ralf Weisse, Corinna Schrum, Ute Daewel, and Lidia Gaslikova
Nat. Hazards Earth Syst. Sci., 23, 1967–1985, https://doi.org/10.5194/nhess-23-1967-2023, https://doi.org/10.5194/nhess-23-1967-2023, 2023
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High seawater levels co-occurring with high river discharges have the potential to cause destructive flooding. For the past decades, the number of such compound events was larger than expected by pure chance for most of the west-facing coasts in Europe. Additionally rivers with smaller catchments showed higher numbers. In most cases, such events were associated with a large-scale weather pattern characterized by westerly winds and strong rainfall.
Alexander Böhme, Birgit Gerkensmeier, Benedikt Bratz, Clemens Krautwald, Olaf Müller, Nils Goseberg, and Gabriele Gönnert
Nat. Hazards Earth Syst. Sci., 23, 1947–1966, https://doi.org/10.5194/nhess-23-1947-2023, https://doi.org/10.5194/nhess-23-1947-2023, 2023
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External surges in the North Sea are caused by low-pressure cells travelling over the northeast Atlantic. They influence extreme water levels on the German coast and have to be considered in the design process of coastal defence structures. This study collects data about external surges from 1995–2020 and analyses their causes, behaviours and potential trends. External surges often occur less than 72 h apart, enabling a single storm surge to be influenced by more than one external surge.
Kenta Tozato, Shuji Moriguchi, Shinsuke Takase, Yu Otake, Michael R. Motley, Anawat Suppasri, and Kenjiro Terada
Nat. Hazards Earth Syst. Sci., 23, 1891–1909, https://doi.org/10.5194/nhess-23-1891-2023, https://doi.org/10.5194/nhess-23-1891-2023, 2023
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This study presents a framework that efficiently investigates the optimal placement of facilities probabilistically based on advanced numerical simulation. Surrogate models for the numerical simulation are constructed using a mode decomposition technique. Monte Carlo simulations using the surrogate models are performed to evaluate failure probabilities. Using the results of the Monte Carlo simulations and the genetic algorithm, optimal placements can be investigated probabilistically.
Job C. M. Dullaart, Sanne Muis, Hans de Moel, Philip J. Ward, Dirk Eilander, and Jeroen C. J. H. Aerts
Nat. Hazards Earth Syst. Sci., 23, 1847–1862, https://doi.org/10.5194/nhess-23-1847-2023, https://doi.org/10.5194/nhess-23-1847-2023, 2023
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Coastal flooding is driven by storm surges and high tides and can be devastating. To gain an understanding of the threat posed by coastal flooding and to identify areas that are especially at risk, now and in the future, it is crucial to accurately model coastal inundation and assess the coastal flood hazard. Here, we present a global dataset with hydrographs that represent the typical evolution of an extreme sea level. These can be used to model coastal inundation more accurately.
Elin Andrée, Jian Su, Morten Andreas Dahl Larsen, Martin Drews, Martin Stendel, and Kristine Skovgaard Madsen
Nat. Hazards Earth Syst. Sci., 23, 1817–1834, https://doi.org/10.5194/nhess-23-1817-2023, https://doi.org/10.5194/nhess-23-1817-2023, 2023
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When natural processes interact, they may compound each other. The combined effect can amplify extreme sea levels, such as when a storm occurs at a time when the water level is already higher than usual. We used numerical modelling of a record-breaking storm surge in 1872 to show that other prior sea-level conditions could have further worsened the outcome. Our research highlights the need to consider the physical context of extreme sea levels in measures to reduce coastal flood risk.
Ekaterina Didenkulova, Ira Didenkulova, and Igor Medvedev
Nat. Hazards Earth Syst. Sci., 23, 1653–1663, https://doi.org/10.5194/nhess-23-1653-2023, https://doi.org/10.5194/nhess-23-1653-2023, 2023
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The paper is dedicated to freak wave accidents which happened in the world ocean in 2005–2021 and that were described in mass media sources. The database accounts for 429 events, all of which resulted in ship or coastal and offshore structure damage and/or human losses. In agreement with each freak wave event, we put background wave and wind conditions extracted from the climate reanalysis ERA5. We analyse their statistics and discuss the favourable conditions for freak wave occurrence.
Havu Pellikka, Milla M. Johansson, Maaria Nordman, and Kimmo Ruosteenoja
Nat. Hazards Earth Syst. Sci., 23, 1613–1630, https://doi.org/10.5194/nhess-23-1613-2023, https://doi.org/10.5194/nhess-23-1613-2023, 2023
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We explore the rate of past and future sea level rise at the Finnish coast, northeastern Baltic Sea, in 1901–2100. For this analysis, we use tide gauge observations, modelling results, and a probabilistic method to combine information from several sea level rise projections. We provide projections of local mean sea level by 2100 as probability distributions. The results can be used in adaptation planning in various sectors with different risk tolerance, e.g. land use planning or nuclear safety.
Carlos Corela, Afonso Loureiro, José Luis Duarte, Luis Matias, Tiago Rebelo, and Tiago Bartolomeu
Nat. Hazards Earth Syst. Sci., 23, 1433–1451, https://doi.org/10.5194/nhess-23-1433-2023, https://doi.org/10.5194/nhess-23-1433-2023, 2023
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We show that ocean-bottom seismometers are controlled by bottom currents, but these are not always a function of the tidal forcing. Instead we suggest that the ocean bottom has a flow regime resulting from two possible contributions: the permanent low-frequency bottom current and the tidal current along the full tidal cycle, between neap and spring tides. In the short-period noise band the ocean current generates harmonic tremors that corrupt the dataset records.
Chen Chen, Charles Koll, Haizhong Wang, and Michael K. Lindell
Nat. Hazards Earth Syst. Sci., 23, 733–749, https://doi.org/10.5194/nhess-23-733-2023, https://doi.org/10.5194/nhess-23-733-2023, 2023
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This paper uses empirical-data-based simulation to analyze how to evacuate efficiently from disasters. We find that departure delay time and evacuation decision have significant impacts on evacuation results. Evacuation results are more sensitive to walking speed, departure delay time, evacuation participation, and destinations than to other variables. This model can help authorities to prioritize resources for hazard education, community disaster preparedness, and resilience plans.
Ariadna Martín, Angel Amores, Alejandro Orfila, Tim Toomey, and Marta Marcos
Nat. Hazards Earth Syst. Sci., 23, 587–600, https://doi.org/10.5194/nhess-23-587-2023, https://doi.org/10.5194/nhess-23-587-2023, 2023
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Tropical cyclones (TCs) are among the potentially most hazardous phenomena affecting the coasts of the Caribbean Sea. This work simulates the coastal hazards in terms of sea surface elevation and waves that originate through the passage of these events. A set of 1000 TCs have been simulated, obtained from a set of synthetic cyclones that are consistent with present-day climate. Given the large number of hurricanes used, robust values of extreme sea levels and waves are computed along the coasts.
An-Chi Cheng, Anawat Suppasri, Kwanchai Pakoksung, and Fumihiko Imamura
Nat. Hazards Earth Syst. Sci., 23, 447–479, https://doi.org/10.5194/nhess-23-447-2023, https://doi.org/10.5194/nhess-23-447-2023, 2023
Short summary
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Consecutive earthquakes occurred offshore of southern Taiwan on 26 December 2006. This event revealed unusual tsunami generation and propagation, as well as unexpected consequences for the southern Taiwanese coast (i.e., amplified waves and prolonged durations). This study aims to elucidate the source characteristics of the 2006 tsunami and the important behaviors responsible for tsunami hazards in Taiwan such as wave trapping and shelf resonance.
Jean Roger, Bernard Pelletier, Aditya Gusman, William Power, Xiaoming Wang, David Burbidge, and Maxime Duphil
Nat. Hazards Earth Syst. Sci., 23, 393–414, https://doi.org/10.5194/nhess-23-393-2023, https://doi.org/10.5194/nhess-23-393-2023, 2023
Short summary
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On 10 February 2021 a magnitude 7.7 earthquake occurring at the southernmost part of the Vanuatu subduction zone triggered a regional tsunami that was recorded on many coastal gauges and DART stations of the south-west Pacific region. Beginning with a review of the tectonic setup and its implication in terms of tsunami generation in the region, this study aims to show our ability to reproduce a small tsunami with different types of rupture models and to discuss a larger magnitude 8.2 scenario.
Kathrin Wahle, Emil V. Stanev, and Joanna Staneva
Nat. Hazards Earth Syst. Sci., 23, 415–428, https://doi.org/10.5194/nhess-23-415-2023, https://doi.org/10.5194/nhess-23-415-2023, 2023
Short summary
Short summary
Knowledge of what causes maximum water levels is often key in coastal management. Processes, such as storm surge and atmospheric forcing, alter the predicted tide. Whilst most of these processes are modeled in present-day ocean forecasting, there is still a need for a better understanding of situations where modeled and observed water levels deviate from each other. Here, we will use machine learning to detect such anomalies within a network of sea-level observations in the North Sea.
Cited articles
Ablain, M., Becker, M., Benveniste, J., Cazenave, A., Champollion, N.,
Ciccarelli, S., Jevrejeva, S., Le Cozannet, G., Nicoletta, L., Loisel, H., Long, N., Maisongrande, P., Mallet, C., Marcos, M., Menendez, M., Meyssignac, B., Plater, A., Raucoules, D., Taramelli, A., Vignudelli, S., Valentini, E., Woodworth, P., and Woppelmann, G.: White paper: Monitoring the evolution of coastal zones under various
forcing factors using space-based observing systems, International Space
Science Institute (ISS), Bern, Switzerland,
available at: https://hal-brgm.archives-ouvertes.fr/hal-01413107 (last access: 5 August 2021), 2016. a
Adloff, F., Somot, S., Sevault, F., Jordà, G., Aznar, R., Déqué,
M., Herrmann, M., Marcos, M., Dubois, C., Padorno, E., Alvarez-Fanjul, E., and Gomis, D.: Mediterranean
Sea response to climate change in an ensemble of twenty first century
scenarios, Clim. Dynam., 45, 2775–2802, https://doi.org/10.1007/s00382-015-2507-3,
2015. a
Alessio, S. M.: Digital signal processing and spectral analysis for scientists:
concepts and applications, Springer, Cham, Switzerland, 2016. a
Allen, M. and Smith, L.: Monte Carlo SSA: Detecting irregular oscillations in
the presence of colored noise, J. Climate, 9, 3373–3404,
https://doi.org/10.1175/1520-0442(1996)009<3373:MCSDIO>2.0.CO;2, 1996. a
Amitai, Y., Ashkenazy, Y., and Gildor, H.: Multiple equilibria and overturning
variability of the Aegean-Adriatic Seas, Global Planet. Change, 151,
49–59, https://doi.org/10.1016/j.gloplacha.2016.05.004, 2017. a
Amorosi, A., Colalongo, M., Fiorini, F., Fusco, F., Pasini, G., Vaiani, S., and
Sarti, G.: Palaeogeographic and palaeoclimatic evolution of the Po Plain from
150-ky core records, Global Planet. Change, 40, 55–78,
https://doi.org/10.1016/S0921-8181(03)00098-5, 2004. a
Androsov, A., Fofonova, V., Kuznetsov, I., Danilov, S., Rakowsky, N., Harig, S., Brix, H., and Wiltshire, K. H.: FESOM-C v.2: coastal dynamics on hybrid unstructured meshes, Geosci. Model Dev., 12, 1009–1028, https://doi.org/10.5194/gmd-12-1009-2019, 2019. a
Antonioli, F., Ferranti, L., Fontana, A., Amorosi, A., Bondesan, A.,
Braitenberg, C., Dutton, A., Fontolan, G., Furlani, S., Lambeck, K., Mastronuzzi, G., Monaco, C., Spada, G., and Stocchi, P.:
Holocene relative sea-level changes and vertical movements along the Italian
and Istrian coastlines, Quaternary Int., 206, 102–133,
https://doi.org/10.1016/j.quaint.2008.11.008, 2009. a, b, c, d, e, f, g, h, i, j
Antonioli, F., Anzidei, M., Amorosi, A., Presti, V. L., Mastronuzzi, G.,
Deiana, G., De Falco, G., Fontana, A., Fontolan, G., Lisco, S., Marsico, A., Moretti, M., Orrù, P. E., Sannino, G., Serpelloni, E., and Vecchio, A.:
Sea-level rise and potential drowning of the Italian coastal plains: Flooding
risk scenarios for 2100, Quat. Sci. Rev., 158, 29–43,
https://doi.org/10.1016/j.quascirev.2016.12.021, 2017. a, b, c, d
Arca, S. and Beretta, G.: Prima sintesi geodetico-geologica sui movimenti
verticali del suolo nell'Italia Settentrionale (1897–1957), Bollettino di
Geodesia e scienze affini, 44, 125–156, 1985. a
Armi, L. and Farmer, D. M.: The flow of Mediterranean water through the strait
of Gibraltar. The flow of Atlantic water through the Strait of Gibraltar,
Prog. Oceanogr., 21, 1–105, 1988. a
Artale, V., Calmanti, S., Malanotte-Rizzoli, P., Pisacane, G., Rupolo, V., and
Tsimplis, M.: The Atlantic and Mediterranean Sea as connected systems, Developments in Earth and Environmental Sciences, 4,
283–323, https://doi.org/10.1016/S1571-9197(06)80008-X, 2006. a
Artale, V., Calmanti, S., Carillo, A., Dell'Aquila, A., Herrmann, M., Pisacane,
G., Ruti, P. M., Sannino, G., Struglia, M. V., Giorgi, F., Bi, X., Pal, J. S., Rauscher, S., and The PROTHEOUS Group: An
atmosphere–ocean regional climate model for the Mediterranean area:
assessment of a present climate simulation, Clim. Dynam., 35, 721–740,
https://doi.org/10.1007/s00382-009-0691-8, 2010. a
Bakker, A. M., Wong, T. E., Ruckert, K. L., and Keller, K.: Sea-level
projections representing the deeply uncertain contribution of the West
Antarctic ice sheet, Sci. Rep., 7, 1–7,
https://doi.org/10.1038/s41598-017-04134-5, 2017. a
Bamber, J. L. and Aspinall, W. P.: An expert judgement assessment of future sea
level rise from the ice sheets, Nat. Clim. Change, 3, 424–427,
https://doi.org/10.1038/nclimate1778, 2013. a
Barriopedro, D., García-Herrera, R., Lionello, P., and Pino, C.: A
discussion of the links between solar variability and high-storm-surge events
in Venice, J. Geophys. Res.-Atmos., 115, D13101, https://doi.org/10.1029/2009JD013114, 2010. a
Benveniste, J., Cazenave, A., Vignudelli, S., Fenoglio-Marc, L., Shah, R.,
Almar, R., Andersen, O. B., Birol, F., Bonnefond, P., Bouffard, J., Calafat, F., Cardellach, E., Cipollini P., Le Cozannet, G., Dufau, C.,
Fernandes, M. J., Frappart, F., Garrison, J., Gommenginger, C., Han, G., Høyer, J. L., Kourafalou, V., Leuliette, E., Li, Z., Loisel, H., Madsen, K. S., Marcos, M.,
Melet, A., Meyssignac, B., Pascual, A., Passaro, M., Ribó, S., Scharroo, R., Song, Y. T., Speich, S., Wilkin, J.,
Woodworth, P., and Wöppelmann, G.:
Requirements for a coastal hazards observing system,
Front. Mar. Sci., 6, 348, https://doi.org/10.3389/fmars.2019.00348, 2019. a
Birol, F., Fuller, N., Lyard, F., Cancet, M., Nino, F., Delebecque, C., Fleury,
S., Toublanc, F., Melet, A., Saraceno, M., and Léger, F.: Coastal applications from
nadir altimetry: Example of the X-TRACK regional products, Adv. Space Res., 59, 936–953, https://doi.org/10.1016/j.asr.2016.11.005, 2017. a, b
Blewitt, G., Hammond, W. C., and Kreemer, C.: Harnessing the GPS data explosion
for interdisciplinary science, Eos, 99, 1–2, https://doi.org/10.1029/2018EO104623,
2018. a, b
Bonaduce, A., Pinardi, N., Oddo, P., Spada, G., and Larnicol, G.: Sea-level
variability in the Mediterranean Sea from altimetry and tide gauges, Clim. Dynam., 47, 2851–2866, https://doi.org/10.1007/s00382-016-3001-2, 2016. a, b
Bondesan, M., Cibin, U., Colalongo, M., Pugliese, N., Stefani, M., Tsakiridis,
E., Vaiani, S., and Vincenzi, S.: Benthic communities and sedimentary facies
recording late Quaternary environmental fluctuations in a Po Delta subsurface
succession (Northern Italy), Proceedings of the 2nd and 3rd Italian Meeting on Environmental Micropaleontology, 11, 21–31, edited by: Coccioni, R., Lirer, F. and Marsili, A., The Grzybowski Foundation Special Publication, 2006. a
Brambati, A., Carbognin, L., Quaia, T., Teatini, P., and Tosi, L.: The Lagoon
of Venice: geological setting, evolution and land subsidence, Episodes, 26,
264–268, https://doi.org/10.18814/epiiugs/2003/v26i3/020, 2003. a, b
Brandt, P., Rubino, A., Sein, D. V., Baschek, B., Izquierdo, A., and Backhaus,
J. O.: Sea level variations in the western Mediterranean studied by a
numerical tidal model of the Strait of Gibraltar, J. Phys. Oceanogr., 34, 433–443,
https://doi.org/10.1175/1520-0485(2004)034<0433:SLVITW>2.0.CO;2, 2004. a
Camuffo, D. and Sturaro, G.: Use of proxy-documentary and instrumental data to
assess the risk factors leading to sea flooding in Venice, Glob. Planet Change, 40, 93–103, https://doi.org/10.1016/S0921-8181(03)00100-0, 2004. a
Carbognin, L., Gatto, P., Mozzi, G., Gambolati, G., and Ricceri, G.: New trend
in the subsidence of Venice, in: Proceedings of the Second International Symposium on Land Subsidence, held at Anaheim, California, 13–17 December 1976, IAHS
Publication, vol. 121, 65–81, edited by: Rodda, J. C., 1976. a, b, c
Carbognin, L., Teatini, P., and Tosi, L.: Eustacy and land subsidence in the
Venice Lagoon at the beginning of the new millennium, J. Marine Syst., 51, 345–353, https://doi.org/10.1016/j.jmarsys.2004.05.021, 2004. a, b
Carbognin, L., Teatini, P., and Tosi, L.: The impact of relative sea level rise
on the Northern Adriatic Sea coast, Italy, WIT Trans. Ecol. Envir., 127, 137–148, https://doi.org/10.2495/RAV090121, 2009. a
Carbognin, L., Teatini, P., Tomasin, A., and Tosi, L.: Global change and
relative sea level rise at Venice: what impact in term of flooding, Clim. Dynam., 35, 1039–1047, https://doi.org/10.1007/s00382-009-0617-5, 2010. a, b, c
Carillo, A., Sannino, G., Artale, V., Ruti, P., Calmanti, S., and Dell'Aquila,
A.: Steric sea level rise over the Mediterranean Sea: present climate and
scenario simulations, Clim. Dynam., 39, 2167–2184,
https://doi.org/10.1007/s00382-012-1369-1, 2012. a
Carminati, E., Doglioni, C., and Scrocca, D.: Apennines subduction-related
subsidence of Venice (Italy), Geophys. Res. Lett., 30, 1717, https://doi.org/10.1029/2003GL017001, 2003. a, b, c
Carminati, E., Enzi, S., and Camuffo, D.: A study on the effects of seismicity
on subsidence in foreland basins: An application to the Venice area, Global Planet. Change, 55, 237–250, https://doi.org/10.1016/j.gloplacha.2006.03.003,
2007. a
Carrère, L. and Lyard, F.: Modeling the barotropic response of the global
ocean to atmospheric wind and pressure forcing-comparisons with observations,
Geophys. Res. Lett., 30, 8–8, https://doi.org/10.1029/2002GL016473, 2003. a
Cazenave, A., Hamlington, B., Horwath, M., Barletta, V. R., Benveniste, J.,
Chambers, D., Döll, P., Hogg, A. E., and Legeais, J. F., Merrifield, M., Meyssignac, B., Mitchum, G., Nerem, S., Pail, R., Palanisamy, H., Paul, F., von Schuckmann, K., and Thompson, P.: Observational requirements for long-term monitoring of the global
mean sea level and its components over the altimetry era, Front. Mar. Sci., 6, 582, https://doi.org/10.3389/fmars.2019.00582, 2019. a, b
Chambers, D. P.: Evaluation of empirical mode decomposition for quantifying multi-decadal variations and acceleration in sea level records, Nonlin. Processes Geophys., 22, 157–166, https://doi.org/10.5194/npg-22-157-2015, 2015. a
Chen, C., Gao, G., Zhang, Y., Beardsley, R. C., Lai, Z., Qi, J., and Lin, H.:
Circulation in the Arctic Ocean: Results from a high-resolution coupled
ice-sea nested Global-FVCOM and Arctic-FVCOM system, Prog. Oceanogr., 141, 60–80, https://doi.org/10.1016/j.pocean.2015.12.002, 2016. a
Church, J. A., Clark, P. U., Cazenave, A., Gregory, J. M., Jevrejeva, S.,
Levermann, A., Merrifield, M. A., Milne, G. A., Nerem, R. S., Nunn, P. D., Payne, A. J., Pfeffer, W. T., Stammer, D., and Unnikrishnan, A. S.: Sea level change, Tech. rep., Climate Change 2013: The Physical
Science Basis. Contribution of Working Group I to the Fifth Assessment Report
of the Intergovernmental Panel on Climate Change, edited by: Stocker, T. F., Qin, D., Plattner, G.-K., Tignor, M., Allen, S. K., Boschung, J., Nauels, A., Xia, Y., Bex, V., and Midgley, P. M., Cambridge University Press, Cambridge, United
Kingdom and New York, NY, USA,
available at: http://drs.nio.org/drs/handle/2264/4605 (last access: 5 August 2021), 2013. a, b
Cipollini, P., Vignudelli, S., Lyard, F., and Roblou, L.: 15 years of altimetry
at various scales over the Mediterranean, 295–306, in: Remote Sensing of the European Seas, edited by: Barale, V. and Gade, M., Springer, Dordrecht, https://doi.org/10.1007/978-1-4020-6772-3_22, 2008. a
Cipollini, P., Passaro, M., and Vignudelli, S.: Validation of Total Water Level
Envelope data from the eSurge processor for Envisat in the North Adriatic
Sea, available at: http://www.storm-surge.info/project-docs (last access: 5 August 2021), 2013. a
Cipollini, P., Benveniste, J., Birol, F., Fernandes, M., Obligis, E., Passaro,
M., Strub, P., Valladeau, G., Vignudelli, S., and Wlikin, J.: Satellite
altimetry in coastal regions, CRC Press, Boca Raton, https://doi.org/10.1201/9781315151779, 2017. a
CNR: Relazione sul pozzo Venezia 1-CNR. 1a fase: Operazioni di cantiere e
analisi delle carote. Laboratorio Dinamica Grandi Masse, Consiglio Nazionale
delle Ricerche, Venice, 1971. a
Criado-Aldeanueva, F., Soto-Navarro, F. J., and García-Lafuente, J.:
Large-scale atmospheric forcing influencing the long-term variability of
Mediterranean heat and freshwater budgets: climatic indices, J. Hydrometeorol., 15, 650–663, https://doi.org/10.1175/JHM-D-13-04.1, 2014. a
Cuffaro, M., Riguzzi, F., Scrocca, D., Antonioli, F., Carminati, E., Livani,
M., and Doglioni, C.: On the geodynamics of the northern Adriatic plate,
Rend. Lincei, 21, 253–279, https://doi.org/10.1007/s12210-010-0098-9, 2010. a, b, c, d
Cusinato, E., Zanchettin, D., Sannino, G., and Rubino, A.: Mediterranean
Thermohaline Response to Large-Scale Winter Atmospheric Forcing in a
High-Resolution Ocean Model Simulation, PApGe, 175, 4083–4110,
https://doi.org/10.1007/s00024-018-1859-0, 2018. a, b
Dangendorf, S., Marcos, M., Wöppelmann, G., Conrad, C. P., Frederikse, T.,
and Riva, R.: Reassessment of 20th century global mean sea level rise,
P. Natl. Acad. Sci. USA, 114, 5946–5951,
https://doi.org/10.1073/pnas.1616007114, 2017. a, b
De Biasio, F., Baldin, G., and Vignudelli, S.: Revisiting Vertical Land Motion
and Sea Level Trends in the Northeastern Adriatic Sea Using Satellite
Altimetry and Tide Gauge Data, Journal of Marine Science and Engineering, 8,
949, https://doi.org/10.3390/jmse8110949, 2020. a
DeConto, R. M. and Pollard, D.: Contribution of Antarctica to past and future
sea-level rise, Nature, 531, 591–597, https://doi.org/10.1038/nature17145, 2016. a
Dodge, Y., Cox, D., Commenges, D., Davison, A., Solomon, P., and Wilson, S. (Eds.): International Statistical Institute, The Oxford dictionary of
statistical terms, Oxford University Press on demand, New York, ISBN 0198509944, 506 pp., 2003. a
Dorigo, L.: Le osservazioni mareografiche in Laguna di Venezia, Ist. Veneto
Sc., Lett. Arti, Commissione di studio dei provvedimenti per la conservazione
e difesa della Laguna e della città di Venezia, Rapporti preliminari,
available at: https://www.beic.it (last access: 5 August 2021), 1961. a, b, c, d
Edwards, T. L., Brandon, M. A., Durand, G., Edwards, N. R., Golledge, N. R.,
Holden, P. B., Nias, I. J., Payne, A. J., Ritz, C., and Wernecke, A.:
Revisiting Antarctic ice loss due to marine ice-cliff instability, Nature,
566, 58–64, https://doi.org/10.1038/s41586-019-0901-4, 2019. a
Environment Agency: Policy paper: Thames Estuary 2100: 10-Year Review
monitoring key findings, Tech. rep., Environment Agency, UK,
available at: https://www.gov.uk/government/publications/thames-estuary-2100-te2100/thames-estuary-2100-key-findings-from-the-monitoring-review, last access: 23 March 2021. a
Erkens, G., Bucx, T., Dam, R., De Lange, G., and Lambert, J.: Sinking coastal
cities, P. Int. Ass. Hydrol. Sci., 372, 189–198, https://doi.org/10.5194/piahs-372-189-2015, 2015. a
Eyring, V., Bony, S., Meehl, G. A., Senior, C. A., Stevens, B., Stouffer, R. J., and Taylor, K. E.: Overview of the Coupled Model Intercomparison Project Phase 6 (CMIP6) experimental design and organization, Geosci. Model Dev., 9, 1937–1958, https://doi.org/10.5194/gmd-9-1937-2016, 2016. a
Ezer, T., Haigh, I. D., and Woodworth, P. L.: Nonlinear sea-level trends and
long-term variability on western European coasts, J. Coast. Res., 32, 744–755, https://doi.org/10.2112/JCOASTRES-D-15-00165.1, 2016. a
Farrell, W. and Clark, J. A.: On postglacial sea level, Geophys. J. Int., 46, 647–667,
https://doi.org/10.1111/j.1365-246X.1976.tb01252.x, 1976. a
Favero, V., Alberotanza, L., and Serandrei Barbero, R.: Aspetti paleoecologici,
sedimentologici e geochimici dei sedimenti attraversati dal pozzo VE 1 bis
CNR Laboratorio per lo Studio della Dinamica delle Grandi Masse, Tech. rep.,
CNR Technical Report 63, Venice, 1973. a
Fernandes, M. J. and Lázaro, C.: GPD+ wet tropospheric corrections for
CryoSat-2 and GFO altimetry missions, Remote Sens., 8, 851,
https://doi.org/10.3390/rs8100851, 2016. a
Ferranti, L., Antonioli, F., Mauz, B., Amorosi, A., Dai Pra, G., Mastronuzzi,
G., Monaco, C., Orrù, P., Pappalardo, M., Radtke, U., Renda, P., Romano, P., Sansò, P., and Verrubbi, V.: Markers of
the last interglacial sea-level high stand along the coast of Italy: tectonic
implications, Quatern. Int., 145, 30–54,
https://doi.org/10.1016/j.quaint.2005.07.009, 2006. a, b, c
Ferrarin, C., Bellafiore, D., Sannino, G., Bajo, M., and Umgiesser, G.: Tidal
dynamics in the inter-connected Mediterranean, Marmara, Black and Azov seas,
Prog. Oceanogr., 161, 102–115, https://doi.org/10.1016/j.pocean.2018.02.006,
2018. a
Flemming, N. C.: Predictions of relative coastal sea-level change in the
Mediterranean based on archaeological, historical and tide-gauge data,
chap. 8, 247–281, in: Climate Change and the Mediterrenean, edited by: Jeftic, L., Millman, J. D., and Sestini, G., 247–281, Edward Arnold, London, 1992. a
Fontana, A., Vinci, G., Tasca, G., Mozzi, P., Vacchi, M., Bivi, G., Salvador,
S., Rossato, S., Antonioli, F., Asioli, A., Bresolin, M., Di Mario, F., and Hajdas, I.: Lagoonal settlements and
relative sea level during Bronze Age in Northern Adriatic: Geoarchaeological
evidence and paleogeographic constraints, Quaternary Int., 439,
17–36, https://doi.org/10.1016/j.quaint.2016.12.038, 2017. a
Fu, L.-L. and Cazenave, A.: Satellite altimetry and earth sciences: a handbook
of techniques and applications, Academic Press, London, 2001. a
Galassi, G. and Spada, G.: Sea-level rise in the Mediterranean Sea by 2050:
Roles of terrestrial ice melt, steric effects and glacial isostatic
adjustment, Global Planet. Change, 123, 55–66,
https://doi.org/10.1016/j.gloplacha.2014.10.007, 2014. a
Galloway, D. and Riley, F. S.: San Joaquin Valley, California, Land subsidence in the United States, Circular 1182, US Geological Survey, 1182, 23–34, 1999. a
Galloway, D. L., Erkens, G., Kuniansky, E. L., and Rowland, J. C.: Preface:
Land subsidence processes, Hydrogeol. J., 24, 547–550,
https://doi.org/10.1007/s10040-016-1386-y, 2016. a
Gambolati, G. and Gatto, P.: Simulazione della subsidenza di Venezia, Venezia
ei problemi dell'ambiente, Il Mulino, Bologna, 299–360, 1975. a
Gambolati, G., Gatto, P., and Freeze, R. A.: Mathematical simulation of the
subsidence of Venice: 2. Results, Water Resour. Res., 10, 563–577,
https://doi.org/10.1029/WR010i003p00563, 1974. a, b, c
Gambolati, G., Teatini, P., and Ferronato, M.: Anthropogenic land subsidence, 2443–2459, in: Encyclopedia of Hydrological Sciences, edited by: Anderson, M. G., John Wiley & Sons, New Jersey, https://doi.org/10.1002/0470848944.hsa164b,
2006. a
García Lafuente, J., Bruque Pozas, E., Sánchez Garrido, J. C., Sannino,
G., and Sammartino, S.: The interface mixing layer and the tidal dynamics at
the eastern part of the Strait of Gibraltar, J. Marine Syst.,
117–118, 31–42, https://doi.org/10.1016/j.jmarsys.2013.02.014, 2013. a
Gómez-Enri, J., González, C., Passaro, M., Vignudelli, S., Álvarez,
O., Cipollini, P., Mañanes, R., Bruno, M., López-Carmona, M., and
Izquierdo, A.: Wind-induced cross-strait sea level variability in the Strait
of Gibraltar from coastal altimetry and in-situ measurements, Remote Sens. Environ., 221, 596–608, https://doi.org/10.1016/j.rse.2018.11.042, 2019. a
Gomis, D., Ruiz, S., Sotillo, M. G., Álvarez-Fanjul, E., and Terradas, J.:
Low frequency Mediterranean sea level variability: the contribution of
atmospheric pressure and wind, Global Planet. Change, 63, 215–229,
https://doi.org/10.1016/j.gloplacha.2008.06.005, 2008. a, b, c
Good, S. A., Martin, M. J., and Rayner, N. A.: EN4: Quality controlled ocean
temperature and salinity profiles and monthly objective analyses with
uncertainty estimates, J. Geophys. Res.-Oceans, 118,
6704–6716, https://doi.org/10.1002/2013JC009067, 2013. a
Gregory, J. M., Griffies, S. M., Hughes, C. W., Lowe, J. A., Church, J. A.,
Fukimori, I., Gomez, N., Kopp, R. E., Landerer, F., Le Cozannet, G., Ponte, R. M., Stammer, D., Tamisiea, M. E., and van de Wal, R. S. W.:
Concepts and terminology for sea level: mean, variability and change, both
local and global, Surv. Geophys., 40, 1251–1289,
https://doi.org/10.1007/s10712-019-09525-z, 2019. a, b, c, d, e, f, g, h
Grinsted, A., Moore, J. C., and Jevrejeva, S.: Application of the cross wavelet transform and wavelet coherence to geophysical time series, Nonlin. Processes Geophys., 11, 561–566, https://doi.org/10.5194/npg-11-561-2004, 2004. a, b, c
Haasnoot, M., Kwadijk, J., Van Alphen, J., Le Bars, D., Van Den Hurk, B.,
Diermanse, F., Van Der Spek, A., Essink, G. O., Delsman, J., and Mens, M.:
Adaptation to uncertain sea-level rise; how uncertainty in Antarctic
mass-loss impacts the coastal adaptation strategy of the Netherlands,
Environ. Res. Lett., 15, 034007, https://doi.org/10.1088/1748-9326/ab666c,
2020. a
Han, W., Stammer, D., Thompson, P., Ezer, T., Palanisamy, H., Zhang, X.,
Domingues, C. M., Zhang, L., and Yuan, D.: Impacts of basin-scale climate
modes on coastal sea level: a review, Surv. Geophys., 40, 1493–1541,
https://doi.org/10.1007/s10712-019-09562-8, 2019. a
Hay, C. C., Morrow, E., Kopp, R. E., and Mitrovica, J. X.: Probabilistic
reanalysis of twentieth-century sea-level rise, Nature, 517, 481–484,
https://doi.org/10.1038/nature14093, 2015. a, b
Hinkel, J., Church, J. A., Gregory, J. M., Lambert, E., Le Cozannet, G., Lowe,
J., McInnes, K. L., Nicholls, R. J., van der Pol, T. D., and van de Wal, R.:
Meeting user needs for sea level rise information: A decision analysis
perspective, Earth's Future, 7, 320–337, https://doi.org/10.1029/2018EF001071, 2019. a
Holt, J., Hyder, P., Ashworth, M., Harle, J., Hewitt, H. T., Liu, H., New, A. L., Pickles, S., Porter, A., Popova, E., Allen, J. I., Siddorn, J., and Wood, R.: Prospects for improving the representation of coastal and shelf seas in global ocean models, Geosci. Model Dev., 10, 499–523, https://doi.org/10.5194/gmd-10-499-2017, 2017. a
Ishii, M., Fukuda, Y., Hirahara, S., Yasui, S., Suzuki, T., and Sato, K.:
Accuracy of global upper ocean heat content estimation expected from present
observational data sets, Sola, 13, 163–167, https://doi.org/10.2151/sola.2017-030,
2017. a
ISPRA: Manuale di mareografia e linee guida per i processi di validazione dei
dati mareografici, Manuali e linee guida 77/2012, ISPRA – Istituto Superiore per la Protezione e la Ricerca Ambientale, Roma, ISBN 978-88-448-0532-6,
2012. a
Jones, P., Jonsson, T., and Wheeler, D.: Extension to the North Atlantic
Oscillation using early instrumental pressure observations from Gibraltar and
South-West Iceland, Int. J. Climatol., 17, 1433–1450,
https://doi.org/10.1002/(SICI)1097-0088(19971115)17:13<1433::AID-JOC203>3.0.CO;2-P,
1997. a
Jordà, G.: Detection time for global and regional sea level trends and
accelerations, J. Geophys. Res.-Oceans, 119, 7164–7174,
https://doi.org/10.1002/2014JC010005, 2014. a, b
Jordà, G. and Gomis, D.: On the interpretation of the steric and mass
components of sea level variability: The case of the Mediterranean basin,
J. Geophys. Res.-Oceans, 118, 953–963,
https://doi.org/10.1002/jgrc.20060, 2013. a, b, c, d
Jordà, G., Gomis, D., and Álvarez-Fanjul, E.: The VANI2-ERA hindcast of
sea-level residuals: atmospheric forcing of sea-level variability in the
Mediterranean Sea (1958–2008), Sci. Mar., 76, 133–146,
https://doi.org/10.3989/scimar.03612.19C, 2012a. a
Jordà, G., Gomis, D., Álvarez-Fanjul, E., and Somot, S.: Atmospheric
contribution to Mediterranean and nearby Atlantic sea level variability under
different climate change scenarios, Global Planet. Change, 80,
198–214, https://doi.org/10.1016/j.gloplacha.2011.10.013, 2012b. a, b
Josey, S. A., Somot, S., and Tsimplis, M.: Impacts of atmospheric modes of
variability on Mediterranean Sea surface heat exchange, J. Geophys. Res.-Oceans, 116, C02032, https://doi.org/10.1029/2010JC006685, 2011. a
Kent, D. V., Rio, D., Massari, F., Kukla, G., and Lanci, L.: Emergence of
Venice during the Pleistocene, Quat. Sci. Rev., 21, 1719–1727,
https://doi.org/10.1016/S0277-3791(01)00153-6, 2002. a, b, c, d
King, M. A., Altamimi, Z., Boehm, J., Bos, M., Dach, R., Elosegui, P., Fund,
F., Hernández-Pajares, M., Lavallee, D., Cerveira, P. J. M., Penna, N., Riva, R. E. M., Steigenberger, P., van Dam, T., Vittuari, L., Williams, S., and Willis, P.:
Improved constraints on models of glacial isostatic adjustment: a review of
the contribution of ground-based geodetic observations, Surv. Geophys., 31, 465–507, https://doi.org/10.1007/s10712-010-9100-4, 2010. a
Kopp, R. E., Horton, R. M., Little, C. M., Mitrovica, J. X., Oppenheimer, M.,
Rasmussen, D., Strauss, B. H., and Tebaldi, C.: Probabilistic 21st and 22nd
century sea-level projections at a global network of tide-gauge sites,
Earth's future, 2, 383–406, https://doi.org/10.1002/2014EF000239, 2014. a, b, c, d, e, f, g, h, i
Kopp, R. E., DeConto, R. M., Bader, D. A., Hay, C. C., Horton, R. M., Kulp, S.,
Oppenheimer, M., Pollard, D., and Strauss, B. H.: Evolving understanding of
Antarctic ice-sheet physics and ambiguity in probabilistic sea-level
projections, Earth's Future, 5, 1217–1233, https://doi.org/10.1002/2017EF000663, 2017. a
Lambeck, K., Antonioli, F., Purcell, A., and Silenzi, S.: Sea-level change
along the Italian coast for the past 10,000 yr, Quat. Sci. Rev.,
23, 1567–1598, https://doi.org/10.1016/j.quascirev.2004.02.009, 2004. a, b
Lambeck, K., Antonioli, F., Anzidei, M., Ferranti, L., Leoni, G., Scicchitano,
G., and Silenzi, S.: Sea level change along the Italian coast during the
Holocene and projections for the future, Quaternary Int., 232,
250–257, https://doi.org/10.1016/j.quaint.2010.04.026, 2011. a, b, c
Landerer, F. W. and Volkov, D. L.: The anatomy of recent large sea level
fluctuations in the Mediterranean Sea, Geophys. Res. Lett., 40,
553–557, https://doi.org/10.1002/grl.50140, 2013. a, b, c, d
Landerer, F. W., Gleckler, P. J., and Lee, T.: Evaluation of CMIP5 dynamic sea
surface height multi-model simulations against satellite observations,
Clim. Dynam., 43, 1271–1283, https://doi.org/10.1007/s00382-013-1939-x, 2014. a
Legeais, J.-F., Ablain, M., Zawadzki, L., Zuo, H., Johannessen, J. A., Scharffenberg, M. G., Fenoglio-Marc, L., Fernandes, M. J., Andersen, O. B., Rudenko, S., Cipollini, P., Quartly, G. D., Passaro, M., Cazenave, A., and Benveniste, J.: An improved and homogeneous altimeter sea level record from the ESA Climate Change Initiative, Earth Syst. Sci. Data, 10, 281–301, https://doi.org/10.5194/essd-10-281-2018, 2018. a, b
Lempert, R.: Robust Decision Making (RDM) BT–Decision Making under Deep
Uncertainty: From Theory to Practice, edited by:
Marchau, V. A. W. J., Walker, W. E., Bloemen, P. J. T. M., and Popper, S. W., Springer, Berlin, 23–51, 2019. a
Lezziero, A.: Indagini paleoambientali nel sottosuolo dell’isola di Burano,
Quaderni di Insula, Venezia, 10, 63–70, 2002. a
Lionello, P.: Extreme storm surges in the gulf of venice: Present and future
climate, Flooding and Environmental Challenges for Venice and its Lagoon:
State of Knowledge, in: Flooding and Environmental Challenges for Venice and its Lagoon: State of Knowledge, edited by: Fletcher, C. A. and Spencer, T., 59–69, Cambridge Univ. Press, New York, 2005. a
Lionello, P., Nicholls, R. J., Umgiesser, G., and Zanchettin, D.: Venice flooding and sea level: past evolution, present issues, and future projections (introduction to the special issue), Nat. Hazards Earth Syst. Sci., 21, 2633–2641, https://doi.org/10.5194/nhess-21-2633-2021, 2021a. a, b, c
Lionello, P., Barriopedro, D., Ferrarin, C., Nicholls, R. J., Orlić, M., Raicich, F., Reale, M., Umgiesser, G., Vousdoukas, M., and Zanchettin, D.: Extreme floods of Venice: characteristics, dynamics, past and future evolution (review article), Nat. Hazards Earth Syst. Sci., 21, 2705–2731, https://doi.org/10.5194/nhess-21-2705-2021, 2021b. a, b, c
Magrini, G. P., De Marchi, L., and Gnesotto, T.: Impianti mareografici eseguiti,
Ricerche Lagunari, available at: https://www.beic.it (last access: 5 August 2021), 1908. a
Marcos, M., Jordà, G., and Le Cozannet, G.: Sea level rise and its impacts
on the Mediterranean, The Mediterranean region under climate change. A
scientific update, IRD Éditions, Marseille, 265–275,
https://doi.org/10.4000/books.irdeditions.22908, 2016. a, b, c
Mariotti, A. and Dell'Aquila, A.: Decadal climate variability in the
Mediterranean region: roles of large-scale forcings and regional processes,
Clim. Dynam., 38, 1129–1145, https://doi.org/10.1007/s00382-011-1056-7, 2012. a
Marshall, J., Kushnir, Y., Battisti, D., Chang, P., Czaja, A., Dickson, R.,
Hurrell, J., McCartney, M., Saravanan, R., and Visbeck, M.: North Atlantic
climate variability: phenomena, impacts and mechanisms, Int. J. Climatol., 21,
1863–1898, https://doi.org/10.1002/joc.693, 2001. a, b
Marti, F., Cazenave, A., Birol, F., Passaro, M., Léger, F., Niño, F.,
Almar, R., Benveniste, J., and Legeais, J. F.: Altimetry-based sea level
trends along the coasts of western Africa, Adv. Space Res., 68, 504–522, https://doi.org/10.1016/j.asr.2019.05.033, 2019. a
Martínez-Asensio, A., Marcos, M., Tsimplis, M. N., Gomis, D., Josey, S.,
and Jordà, G.: Impact of the atmospheric climate modes on Mediterranean
sea level variability, Global Planet. Change, 118, 1–15,
https://doi.org/10.1016/j.gloplacha.2014.03.007, 2014. a
Martínez-Asensio, A., Tsimplis, M. N., and Calafat, F. M.: Decadal
variability of European sea level extremes in relation to the solar activity,
Geophys. Res. Lett., 43, 11–744, https://doi.org/10.1002/2016GL071355, 2016. a
Maslova, V. N., Voskresenskaya, E. N., and Lubkov, A. S.: Multidecadal change
of winter cyclonic activity in the Mediterranean associated with AMO and
PDO, Terr. Atmos. Ocean. Sci., 28, 965–977, https://doi.org/10.3319/TAO.2017.04.23.01, 2017. a
Massari, F., Rio, D., Barbero, R. S., Asioli, A., Capraro, L., Fornaciari, E.,
and Vergerio, P.: The environment of Venice area in the past two million
years, Palaeogeogr. Palaeocl., 202, 273–308,
https://doi.org/10.1016/S0031-0182(03)00640-0, 2004. a, b
Melini, D. and Spada, G.: Some remarks on Glacial Isostatic Adjustment
modelling uncertainties, Geophys. J. Int., 218, 401–413,
https://doi.org/10.1093/gji/ggz158, 2019. a
Menemenlis, D., Fukumori, I., and Lee, T.: Atlantic to Mediterranean sea level
difference driven by winds near Gibraltar Strait, J. Phys. Oceanogr., 37, 359–376, https://doi.org/10.1175/JPO3015.1, 2007. a
Meyssignac, B., Slangen, A. A., Melet, A., Church, J., Fettweis, X., Marzeion,
B., Agosta, C., Ligtenberg, S., Spada, G., Richter, K., Palmer, M. D., Roberts, C. D., and Champollion, N.: Evaluating
model simulations of twentieth-century sea-level rise. Part II: Regional
sea-level changes, J. Climate, 30, 8565–8593,
https://doi.org/10.1175/JCLI-D-17-0112.1, 2017. a
Milne, G. A., Gehrels, W. R., Hughes, C. W., and Tamisiea, M. E.: Identifying
the causes of sea-level change, Nat. Geosci., 2, 471–478,
https://doi.org/10.1038/ngeo544, 2009. a
Mitrovica, J. X., Gomez, N., and Clark, P. U.: The sea-level fingerprint of
West Antarctic collapse, Science, 323, 753–753,
https://doi.org/10.1126/science.1166510, 2009. a
Naranjo, C., Garcia-Lafuente, J., Sannino, G., and Sanchez-Garrido, J.: How
much do tides affect the circulation of the Mediterranean Sea? From local
processes in the Strait of Gibraltar to basin-scale effects, Prog. Oceanogr., 127, 108–116, https://doi.org/10.1016/j.pocean.2014.06.005, 2014. a
Nicholls, R. J., Hanson, S. E., Lowe, J. A., Warrick, R. A., Lu, X., and Long,
A. J.: Sea-level scenarios for evaluating coastal impacts, WIRES Clim. Change, 5, 129–150,
https://doi.org/10.1002/wcc.253, 2014. a, b
Nicholls, R. J., Hanson, S. E., Lowe, J. A., Slangen, A. B., Wahl, T., Hinkel,
J., and Long, A. J.: Integrating new sea-level scenarios into coastal risk
and adaptation assessments: An ongoing process, WIRES Clim. Change, 12, e706, https://doi.org/10.1002/wcc.706, 2021. a, b
Oppenheimer, M., Glavovic, B., Hinkel, J., van de Wal, R., Magnan, A. K.,
Abd-Elgawad, A., Cai, R., Cifuentes-Jara, M., Deconto, R. M., Ghosh, T., Hay, J., Isla, F., Marzeion, B., Meyssignac, B., and Sebesvari, Z.: Sea level rise and implications for low lying islands, coasts and
communities, in: IPCC Special Report on the
Ocean and Cryosphere in a Changing Climate, edited by: Roberts, D. C., Masson-Delmotte, V., Zhai, P., Tignor, M., Poloczanska, E., Mintenbeck, K., Alegría, A., Nicolai, M., Okem, A., Petzold, J., Rama, B., and Weyer, N. M., Cambridge University Press,
Cambridge, UK, 2019. a, b, c, d
Palma, M., Iacono, R., Sannino, G., Bargagli, A., Carillo, A., Fekete, B. M.,
Lombardi, E., Napolitano, E., Pisacane, G., and Struglia, M. V.: Short-term,
linear, and non-linear local effects of the tides on the surface dynamics in
a new, high-resolution model of the Mediterranean Sea circulation, Ocean
Dynam., 70, 935–963, https://doi.org/10.1007/s10236-020-01364-6, 2020. a
Parras-Berrocal, I. M., Vazquez, R., Cabos, W., Sein, D., Mañanes, R., Perez-Sanz, J., and Izquierdo, A.: The climate change signal in the Mediterranean Sea in a regionally coupled atmosphere–ocean model, Ocean Sci., 16, 743–765, https://doi.org/10.5194/os-16-743-2020, 2020. a
Peltier, W. R.: Global glacial isostasy and the surface of the ice-age Earth:
the ICE-5G (VM2) model and GRACE, Annu. Rev. Earth Planet. Sci., 32,
111–149, https://doi.org/10.1146/annurev.earth.32.082503.144359, 2004. a
Piecuch, C. G., Dangendorf, S., Gawarkiewicz, G. G., Little, C. M., Ponte,
R. M., and Yang, J.: How is New England coastal sea level related to the
Atlantic meridional overturning circulation at 26∘ N?, Geophys. Res. Lett., 46, 5351–5360, https://doi.org/10.1029/2019GL083073, 2019. a, b
Pirazzoli, P.: Sea level changes. The last 2000 years, John Wiley & Sons, Chichester, 211 pp., 1996. a
Pisacane, G., Artale, V., Calmanti, S., and Rupolo, V.: Decadal oscillations in
the Mediterranean Sea: a result of the overturning circulation variability in
the eastern basin?, Clim. Res., 31, 257–271, https://doi.org/10.3354/cr031257,
2006. a
Polli, S.: Il graduale aumento del livello del mare lungo le coste italiane,
Geofisica pura e applicata, 25, 123–129, https://doi.org/10.1007/BF02014061, 1953. a
Polyakov, I. V., Pnyushkov, A. V., and Timokhov, L. A.: Warming of the
Intermediate Atlantic Water of the Arctic Ocean in the 2000s, J. Climate, 25, 8362–8370, https://doi.org/10.1175/JCLI-D-12-00266.1, 2012. a
Ponte, R. M., Carson, M., Cirano, M., Domingues, C. M., Jevrejeva, S., Marcos,
M., Mitchum, G., van de Wal, R. S. W., Woodworth, P. L., Ablain, M., Ardhuin,
F., Ballu, V., Becker, M., Benveniste, J., Birol, F., Bradshaw, E., Cazenave,
A., De Mey-Frémaux, P., Durand, F., Ezer, T., Fu, L.-L., Fukumori, I.,
Gordon, K., Gravelle, M., Griffies, S. M., Han, W., Hibbert, A., Hughes,
C. W., Idier, D., Kourafalou, V. H., Little, C. M., Matthews, A., Melet, A.,
Merrifield, M., Meyssignac, B., Minobe, S., Penduff, T., Picot, N., Piecuch,
C., Ray, R. D., Rickards, L., Santamaría-Gómez, A., Stammer, D., Staneva,
J., Testut, L., Thompson, K., Thompson, P., Vignudelli, S., Williams, J.,
Williams, S. D. P., Wöppelmann, G., Zanna, L., and Zhang, X.: Towards
comprehensive observing and modeling systems for monitoring and predicting
regional to coastal sea level, Front. Mar. Sci., 6, 437, https://doi.org/10.3389/fmars.2019.00437, 2019. a
Quartly, G. D., Legeais, J.-F., Ablain, M., Zawadzki, L., Fernandes, M. J., Rudenko, S., Carrère, L., García, P. N., Cipollini, P., Andersen, O. B., Poisson, J.-C., Mbajon Njiche, S., Cazenave, A., and Benveniste, J.: A new phase in the production of quality-controlled sea level data, Earth Syst. Sci. Data, 9, 557–572, https://doi.org/10.5194/essd-9-557-2017, 2017. a
Ranger, N., Reeder, T., and Lowe, J.: Addressing “deep” uncertainty over
long-term climate in major infrastructure projects: four innovations of the
Thames Estuary 2100 Project, EURO Journal on Decision Processes, 1, 233–262,
https://doi.org/10.1007/s40070-013-0014-5, 2013. a
Roy, K. and Peltier, W. R.: Relative sea level in the Western Mediterranean
basin: a regional test of the ICE-7G_NA (VM7) model and a constraint on late
Holocene Antarctic deglaciation, Quat. Sci. Rev., 183, 76–87,
https://doi.org/10.1016/j.quascirev.2017.12.021, 2018. a
Rubino, A., Zanchettin, D., Androsov, A., and Voltzinger, N. E.: Tidal Records
as Liquid Climate Archives for Large-Scale Interior Mediterranean
Variability, Sci. Rep., 8, 1–8, https://doi.org/10.1038/s41598-018-30930-8,
2018. a
Rusconi, A.: Il Comune Marino a Venezia: ricerche e ipotesi sulle sue
variazioni altimetriche e sui fenomeni naturali che le determinano, Ufficio Idrografico Magistrato Acque, Venice, Italy, Pubbl., 157, 39, 1983. a
Salvioni, G.: I movimenti del suolo nell'Italia centro-settentrionale,
Bollettino di geodesia e scienze affini, 16, 325–366, 1957. a
Sánchez, L., Völksen, C., Sokolov, A., Arenz, H., and Seitz, F.: Present-day surface deformation of the Alpine region inferred from geodetic techniques, Earth Syst. Sci. Data, 10, 1503–1526, https://doi.org/10.5194/essd-10-1503-2018, 2018. a
Sannino, G., Pratt, L., and Carillo, A.: Hydraulic criticality of the exchange
flow through the Strait of Gibraltar, J. Phys. Oceanogr., 39,
2779–2799, https://doi.org/10.1175/2009JPO4075.1, 2009. a
Sannino, G., Carillo, A., Pisacane, G., and Naranjo, C.: On the relevance of
tidal forcing in modelling the Mediterranean thermohaline circulation,
Prog. Oceanogr., 134, 304–329, https://doi.org/10.1016/j.pocean.2015.03.002,
2015. a
Santamaría-Gómez, A., Gravelle, M., Dangendorf, S., Marcos, M., Spada,
G., and Wöppelmann, G.: Uncertainty of the 20th century sea-level rise
due to vertical land motion errors, Earth Planet. Sci. Lett., 473,
24–32, https://doi.org/10.1016/j.epsl.2017.05.038, 2017. a, b, c
Scafetta, N.: Multi-scale dynamical analysis (MSDA) of sea level records versus
PDO, AMO, and NAO indexes, Clim. Dynam., 43, 175–192,
https://doi.org/10.1007/s00382-013-1771-3, 2014. a
Scharroo, R., Leuliette, E., Lillibridge, J., Byrne, D., Naeije, M., and
Mitchum, G.: RADS: Consistent Multi-Mission Products, ESASP, in Proceedings
of the Symposium on 20 Years of Progress in Radar Altimetry, 24–29 September
2012, Special Publication SP-710, p. 69, European Space Agency, Venice,
Italy, 2013. a
Sein, D. V., Mikolajewicz, U., Gröger, M., Fast, I., Cabos, W., Pinto,
J. G., Hagemann, S., Semmler, T., Izquierdo, A., and Jacob, D.: Regionally
coupled atmosphere-ocean-sea ice-marine biogeochemistry model ROM: 1.
Description and validation, J. Adv. Model. Earth Sy., 7,
268–304, https://doi.org/10.1002/2014MS000357, 2015. a
Serandrei Barbero, R., Lezziero, A., Albani, A., and Zoppi, U.: Depositi
tardo-pleistocenici ed olocenici nel sottosuolo veneziano: paleoambienti e
cronologia, Il Quaternario, 14, 9–22, 2001. a
Simoncelli, S., Fratianni, C., Pinardi, N., Grandi, A., Drudi, M., and Oddo,
P.: Mediterranean Sea physical reanalysis (MEDREA 1987–2017) (Version 1),
Copernicus Monitoring Environment Marine Service (CMEMS) [data set],
https://doi.org/10.25423/medsea_reanalysis_phys_006_004, 2014. a
Slangen, A., Katsman, C., Van de Wal, R., Vermeersen, L., and Riva, R.: Towards
regional projections of twenty-first century sea-level change based on IPCC
SRES scenarios, Clim. Dynam., 38, 1191–1209,
https://doi.org/10.1007/s00382-011-1057-6, 2012. a, b
Slangen, A., Carson, M., Katsman, C., Van de Wal, R., Köhl, A., Vermeersen,
L., and Stammer, D.: Projecting twenty-first century regional sea-level
changes, Clim. Change, 124, 317–332, https://doi.org/10.1007/s10584-014-1080-9,
2014. a
Slangen, A., Adloff, F., Jevrejeva, S., Leclercq, P., Marzeion, B., Wada, Y.,
and Winkelmann, R.: A review of recent updates of sea-level projections at
global and regional scales, Surv. Geophys., 38, 385–406,
https://doi.org/10.1007/s10712-016-9374-2, 2017. a, b
Slangen, A. B., Church, J. A., Agosta, C., Fettweis, X., Marzeion, B., and
Richter, K.: Anthropogenic forcing dominates global mean sea-level rise since
1970, Nat. Clim. Change, 6, 701–705, https://doi.org/10.1038/nclimate2991, 2016. a
Slivinski, L. C., Compo, G. P., Whitaker, J. S., Sardeshmukh, P. D., Giese,
B. S., McColl, C., Allan, R., Yin, X., Vose, R., Titchner, H., Kennedy, J., Spencer, L. J., Ashcroft, L., Brönnimann, S., Brunet, M., Camuffo, D., Cornes, R., Cram, T. A., Crouthamel, R., Domínguez-Castro, F., Freeman, J. E., Gergis, J., Hawkins, E., Jones, P. D., Jourdain, S., Kaplan, A., Kubota, H., Le Blancq, F., Lee, T.-C., Lorrey, A., Luterbacher, J., Maugeri, M., Mock, C. J., Moore, G. W. K., Przybylak, R., Pudmenzky, C., Reason, C., Slonosky, V. C., Smith, C. A., Tinz, B., Trewin, B., Valente, M. A., Wang, X. L., Wilkinson, C., Wood, K., and Wyszyński, P.:
Towards a more reliable historical reanalysis: Improvements for version 3 of
the Twentieth Century Reanalysis system, Q. J. Roy. Meteor. Soc., 145, 2876–2908, https://doi.org/10.1002/qj.3598, 2019. a
Somot, S., Sevault, F., Déqué, M., and Crépon, M.: 21st century
climate change scenario for the Mediterranean using a coupled
atmosphere–ocean regional climate model, Global Planet. Change, 63,
112–126, https://doi.org/10.1016/j.gloplacha.2007.10.003, 2008. a
Spada, G.: Glacial isostatic adjustment and contemporary sea level rise: An
overview, Surv. Geophys., 38, 153–185,
https://doi.org/10.1007/s10712-016-9379-x, 2017. a
Spada, G. and Melini, D.: On Some Properties of the Glacial Isostatic
Adjustment Fingerprints, Water, 11, 1844, https://doi.org/10.3390/w11091844, 2019. a
Spada, G., Stocchi, P., and Colleoni, F.: Glacio–isostatic adjustment in the
po plain and in the northern adriatic region, Pure Appl. Geophys.,
166, 1303–1318, https://doi.org/10.1007/s00024-004-0498-9, 2009. a
Spada, G., Bamber, J., and Hurkmans, R.: The gravitationally consistent
sea-level fingerprint of future terrestrial ice loss, Geophys. Res. Lett., 40, 482–486, https://doi.org/10.1029/2012GL053000, 2013. a
Stammer, D. and Cazenave, A.: Satellite altimetry over oceans and land
surfaces, CRC Press, Boca Raton, https://doi.org/10.1201/9781315151779, 2017. a
Stocchi, P. and Spada, G.: Influence of glacial isostatic adjustment upon
current sea level variations in the Mediterranean, Tectonophysics, 474,
56–68, https://doi.org/10.1016/j.tecto.2009.01.003, 2009. a
Stocchi, P., Spada, G., and Cianetti, S.: Isostatic rebound following the
Alpine deglaciation: impact on the sea level variations and vertical
movements in the Mediterranean region, Geophys. J. Int.,
162, 137–147, https://doi.org/10.1111/j.1365-246X.2005.02653.x, 2005. a
Tambroni, N. and Seminara, G.: Are inlets responsible for the morphological
degradation of Venice Lagoon?, J. Geophys. Res.-Earth, 111, F03013, https://doi.org/10.1029/2005JF000334, 2006. a
Taricco, C., Alessio, S., Rubinetti, S., Zanchettin, D., Cosoli, S.,
Gačić, M., Mancuso, S., and Rubino, A.: Marine Sediments Remotely
Unveil Long-Term Climatic Variability Over Northern Italy, Sci. Rep., 5, 12111, https://doi.org/10.1038/srep12111, 2015. a
Teatini, P., Ferronato, M., Gambolati, G., Bertoni, W., and Gonella, M.: A
century of land subsidence in Ravenna, Italy, Environ. Geol., 47,
831–846, https://doi.org/10.1007/s00254-004-1215-9, 2005. a
Teatini, P., Tosi, L., Strozzi, T., Carbognin, L., Cecconi, G., Rosselli, R.,
and Libardo, S.: Resolving land subsidence within the Venice Lagoon by
persistent scatterer SAR interferometry, Phys. Chem. Earth PT A/B/C, 40, 72–79, https://doi.org/10.1016/j.pce.2010.01.002, 2012. a
Thiéblemont, R., Le Cozannet, G., Toimil, A., Meyssignac, B., and Losada,
I. J.: Likely and High-End Impacts of Regional Sea-Level Rise on the
Shoreline Change of European Sandy Coasts Under a High Greenhouse Gas
Emissions Scenario, Water, 11, 2607, https://doi.org/10.3390/w11122607, 2019. a, b, c, d, e
Torge, W. and Müller, J.: Geodesy, Walter de Gruyter, Berlin, Germany, 1980. a
Tosi, L., Teatini, P., Carbognin, L., and Brancolini, G.: Using high resolution
data to reveal depth-dependent mechanisms that drive land subsidence: The
Venice coast, Italy, Tectonophysics, 1, 271–284,
https://doi.org/10.1016/j.tecto.2009.02.026, 2009. a, b
Tosi, L., Teatini, P., Strozzi, T., Carbognin, L., Brancolini, G., and
Rizzetto, F.: Ground surface dynamics in the northern Adriatic coastland over
the last two decades, Rend. Lincei, 21, 115–129,
https://doi.org/10.1007/s12210-010-0084-2, 2010. a
Troccoli, A., Zambon, F., Hodges, K. I., and Marani, M.: Storm surge frequency
reduction in Venice under climate change, Clim. Change, 113, 1065–1079,
https://doi.org/10.1007/s10584-011-0093-x, 2012. a, b
Tsimplis, M., Álvarez-Fanjul, E., Gomis, D., Fenoglio-Marc, L., and
Pérez, B.: Mediterranean sea level trends: atmospheric pressure and wind
contribution, Geophys. Res. Lett., 32, L20602, https://doi.org/10.1029/2005GL023867,
2005. a
Tsimplis, M., Shaw, A., Flather, R., and Woolf, D.: The influence of the North
Atlantic Oscillation on the sea-level around the northern European coasts
reconsidered: the thermosteric effects, Philos. T. Roy. Soc. A, 364,
845–856, https://doi.org/10.1098/rsta.2006.1740, 2006. a
Tsimplis, M., Calafat, F. M., Marcos, M., Jordá, G., Gomis, D.,
Fenoglio-Marc, L., Struglia, M., Josey, S. A., and Chambers, D.: The effect
of the NAO on sea level and on mass changes in the Mediterranean Sea, J. Geophys. Res.-Oceans, 118, 944–952, https://doi.org/10.1002/jgrc.20078,
2013. a, b, c
Tsimplis, M. N. and Baker, T. F.: Sea level drop in the Mediterranean Sea: an
indicator of deep water salinity and temperature changes?, Geophys. Res. Lett., 27, 1731–1734, https://doi.org/10.1029/1999GL007004, 2000. a, b
Tsimplis, M. N. and Shaw, A. G.: The forcing of mean sea level variability
around Europe, Global Planet. Change, 63, 196–202,
https://doi.org/10.1016/j.gloplacha.2007.08.018, 2008. a, b
Tsimplis, M. N., Marcos, M., and Somot, S.: 21st century Mediterranean sea
level rise: steric and atmospheric pressure contributions from a regional
model, Global Planet. Change, 63, 105–111,
https://doi.org/10.1016/j.gloplacha.2007.09.006, 2008. a, b, c
Turuncoglu, U. U. and Sannino, G.: Validation of newly designed regional earth
system model (RegESM) for Mediterranean Basin, Clim. Dynam., 48,
2919–2947, https://doi.org/10.1007/s00382-016-3241-1, 2017. a
Umgiesser, G., Bajo, M., Ferrarin, C., Cucco, A., Lionello, P., Zanchettin, D., Papa, A., Tosoni, A., Ferla, M., Coraci, E., Morucci, S., Crosato, F., Bonometto, A., Valentini, A., Orlić, M., Haigh, I. D., Nielsen, J. W., Bertin, X., Fortunato, A. B., Pérez Gómez, B., Alvarez Fanjul, E., Paradis, D., Jourdan, D., Pasquet, A., Mourre, B., Tintoré, J., and Nicholls, R. J.: The prediction of floods in Venice: methods, models and uncertainty (review article), Nat. Hazards Earth Syst. Sci., 21, 2679–2704,
https://doi.org/10.5194/nhess-21-2679-2021, 2021. a, b
UNESCO: General Concepts, UNESCO Land Subsidence International Initiative,
available at: https://www.landsubsidence-unesco.org/general-concepts/ (last access: 5 August 2021),
2020. a
Vecchio, A., Anzidei, M., Serpelloni, E., and Florindo, F.: Natural Variability
and Vertical Land Motion Contributions in the Mediterranean Sea-Level Records
over the Last Two Centuries and Projections for 2100, Water, 11, 1480,
https://doi.org/10.3390/w11071480, 2019. a, b, c, d
Vignudelli, S.: Analysis of ERS-1 altimeter collinear passes in the
Mediterranean Sea during 1992–1993, Int. J. Remote Sens.,
18, 573–601, https://doi.org/10.1080/014311697218953, 1997. a
Vignudelli, S., Kostianoy, A. G., Cipollini, P., and Benveniste, J.: Coastal
altimetry, Springer, Berlin, Heidelberg, https://doi.org/10.1007/978-3-642-12796-0, 2011. a
Vignudelli, S., Birol, F., Benveniste, J., Fu, L.-L., Picot, N., Raynal, M.,
and Roinard, H.: Satellite altimetry measurements of sea level in the coastal
zone, Surv. Geophys., 40, 1319–1349,
https://doi.org/10.1007/s10712-019-09569-1, 2019a. a, b
Whitehouse, P. L.: Glacial isostatic adjustment modelling: historical perspectives, recent advances, and future directions, Earth Surf. Dynam., 6, 401–429, https://doi.org/10.5194/esurf-6-401-2018, 2018. a
Williams, S. D.: CATS: GPS coordinate time series analysis software, GPS
solutions, 12, 147–153, https://doi.org/10.1007/s10291-007-0086-4, 2008. a, b
Woodworth, P. L., Pouvreau, N., and Wöppelmann, G.: The gyre-scale circulation of the North Atlantic and sea level at Brest, Ocean Sci., 6, 185–190, https://doi.org/10.5194/os-6-185-2010, 2010. a
Woodworth, P. L.: Differences between mean tide level and mean sea level,
J. Geodesy, 91, 69–90, https://doi.org/10.1007/s00190-016-0938-1, 2017. a
Wöppelmann, G. and Marcos, M.: Coastal sea level rise in southern Europe
and the nonclimate contribution of vertical land motion, J. Geophys. Res.-Oceans, 117, C01007, https://doi.org/10.1029/2011JC007469, 2012. a, b, c, d
Wöppelmann, G. and Marcos, M.: Vertical land motion as a key to
understanding sea level change and variability, Rev. Geophys., 54,
64–92, https://doi.org/10.1002/2015RG000502, 2016. a, b, c
Wöppelmann, G., Zerbini, S., and Marcos, M.: Tide gauges and Geodesy: a
secular synergy illustrated by three present-day case studies, C. R. Geosci., 338, 980–991, https://doi.org/10.1016/j.crte.2006.07.006, 2006. a
Wöppelmann, G., Marcos, M., Coulomb, A., Míguez, B. M., Bonnetain, P.,
Boucher, C., Gravelle, M., Simon, B., and Tiphaneau, P.: Rescue of the
historical sea level record of Marseille (France) from 1885 to 1988 and its
extension back to 1849–1851, J. Geodesy, 88, 869–885,
https://doi.org/10.1007/s00190-014-0728-6, 2014. a
Zanchettin, D.: Aerosol and solar irradiance effects on decadal climate
variability and predictability, Current Climate Change Reports, 3, 150–162,
https://doi.org/10.1007/s40641-017-0065-y, 2017. a
Zanchettin, D., Rubino, A., Traverso, P., and Tomasino, M.: Impact of
variations in solar activity on hydrological decadal patterns in northern
Italy, J. Geophys. Res.-Atmos., 113, D12102, https://doi.org/10.1029/2007JD009157, 2008. a
Zanchettin, D., Bothe, O., Rubino, A., and Jungclaus, J. H.: Multi-model
ensemble analysis of Pacific and Atlantic SST variability in unperturbed
climate simulations, Clim. Dynam., 47, 1073–1090,
https://doi.org/10.1007/s00382-015-2889-2, 2016.
a
Zanchettin, D., Bruni, S., Thiéblemont, R., and Rubinetti, S.: Data from article “Sea-level rise in Venice: historic and future trends (review article)”, Zenodo [data set], https://doi.org/10.5281/zenodo.5139890, 2021. a
Zanna, L., Khatiwala, S., Gregory, J. M., Ison, J., and Heimbach, P.: Global
reconstruction of historical ocean heat storage and transport, P. Natl. Acad. Sci. USA, 116, 1126–1131,
https://doi.org/10.1073/pnas.1808838115, 2019. a
Zerbini, S., Raicich, F., Prati, C. M., Bruni, S., Del Conte, S., Errico, M.,
and Santi, E.: Sea-level change in the Northern Mediterranean Sea from
long-period tide gauge time series, Earth-Sci. Rev., 167, 72–87,
https://doi.org/10.1016/j.earscirev.2017.02.009, 2017. a, b, c, d, e, f, g, h, i, j, k, l, m, n, o, p, q, r, s
Zezza, F.: The sedimentary structure of Upper Pleistocene–Holocene deposits in
Venice and its effects on the stability of the historic centre, Rend.
Lincei, 21, 211–227, https://doi.org/10.1007/s12210-010-0089-x, 2010. a
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Relative sea level in Venice rose by about 2.5 mm/year in the past 150 years due to the combined effect of subsidence and mean sea-level rise. We estimate the likely range of mean sea-level rise in Venice by 2100 due to climate changes to be between about 10 and 110 cm, with an improbable yet possible high-end scenario of about 170 cm. Projections of subsidence are not available, but historical evidence demonstrates that they can increase the hazard posed by climatically induced sea-level rise.
Relative sea level in Venice rose by about 2.5 mm/year in the past 150 years due to the combined...
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