Articles | Volume 16, issue 12
Nat. Hazards Earth Syst. Sci., 16, 2799–2822, 2016
Nat. Hazards Earth Syst. Sci., 16, 2799–2822, 2016

Research article 21 Dec 2016

Research article | 21 Dec 2016

Typhoon Haiyan's sedimentary record in coastal environments of the Philippines and its palaeotempestological implications

Dominik Brill1, Simon Matthias May1, Max Engel1, Michelle Reyes2, Anna Pint1, Stephan Opitz1, Manuel Dierick3, Lia Anne Gonzalo4, Sascha Esser1, and Helmut Brückner1 Dominik Brill et al.
  • 1Institute of Geography, Universität zu Köln, Cologne, Germany
  • 2Marine Science Institute, University of the Philippines, Quezon City, Philippines
  • 3Department of Physics and Astronomy, Ghent University, Ghent, Belgium
  • 4Nationwide Operational Assessment of Hazards (Project NOAH), Department of Science and Technology, Quezon City, Philippines

Abstract. On 8 November 2013, category 5 Supertyphoon Haiyan made landfall on the Philippines. During a post-typhoon survey in February 2014, Haiyan-related sand deposition and morphological changes were documented at four severely affected sites with different exposure to the typhoon track and different geological and geomorphological settings. Onshore sand sheets reaching 100–250 m inland are restricted to coastal areas with significant inundation due to amplification of surge levels in embayments or due to accompanying long-wave phenomena at the most exposed coastlines of Leyte and Samar. However, localized washover fans with a storm-typical laminated stratigraphy occurred even along coasts with limited inundation due to waves overtopping or breaching coastal barriers. On a recent reef platform off Negros in the Visayan Sea, storm waves entrained coral rubble from the reef slope and formed an intertidal coral ridge several hundreds of metres long when breaking at the reef edge. As these sediments and landforms were generated by one of the strongest storms ever recorded, they not only provide a recent reference for typhoon signatures that can be used for palaeotempestological and palaeotsunami studies in the region but might also increase the general spectrum of possible cyclone deposits. Although a rather atypical example for storm deposition due to the influence of infra-gravity waves, it nevertheless provides a valuable reference for an extreme case that should be considered when discriminating between storm and tsunami deposits in general. Even for sites with low topography and high inundation levels during Supertyphoon Haiyan, the landward extent of the documented sand sheets seems significantly smaller than typical sand sheets of large tsunamis. This criterion may potentially be used to distinguish both types of events.

Short summary
Sediments and landforms related to Typhoon Haiyan were documented for coastal settings on the Philippines. Sand sheets are restricted to coasts with strong inundation, while washover fans due to overtopping waves were more abundant. Wave-generated coral ridges are reported from an intertidal reef platform. As generated by an exceptional storm, documented signatures like the limited landward extent of sand sheets may potentially help to distinguish storm and tsunami in the geological record.
Final-revised paper