the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
06 Jan 2021
06 Jan 2021
Investigating 3D and 4D Variational Rapid-Update-Cycling Assimilation of Weather Radar Reflectivity for a Flash Flood Event in Central Italy
- 1Centre of Excellence CETEMPS, Department of Physical and Chemical Sciences – University of L’Aquila, L’Aquila, 67100, Italy
- 2Department of Information Engineering, Sapienza University of Rome, Rome, 00185, Italy
- 1Centre of Excellence CETEMPS, Department of Physical and Chemical Sciences – University of L’Aquila, L’Aquila, 67100, Italy
- 2Department of Information Engineering, Sapienza University of Rome, Rome, 00185, Italy
Abstract. The precipitation forecast over the Mediterranean basin is still a challenge because of the complex orographic region which amplifies the need for local observation to correctly initialize the forecast. In this context the data assimilation techniques play a key role in improving the initial conditions and consequently the timing and position of precipitation pattern. For the first time, the ability of a cycling 4D-Var to reproduce a severe weather event in central Italy, as well as to provide a comparison with the largely used cycling 3D-Var, is evaluated in this study. The radar reflectivity measured by the Italian ground radar network is assimilated in the WRF model to simulate an event occurred on May 3, 2018 in central Italy. In order to evaluate the impact of data assimilation, several simulations are objectively compared by means of a Fraction Skill Score (FSS), which is calculated for several threshold values, and a Receiver Operating Characteristic (ROC) curve. The results suggest that both assimilation methods in cycling mode improve the 1, 3 and 6-hourly quantitative precipitation estimation. More specifically, the cycling 4D-Var with a warm start initialization shows the highest FSS values in the first hours of simulation both with light and heavy precipitation. Finally, the ROC curve confirms the benefit of 4D-Var: the area under the curve is 0.91 compared to the 0.88 of control experiment without data assimilation.
Vincenzo Mazzarella et al.
Status: final response (author comments only)
-
RC1: 'Comment on nhess-2020-406', Anonymous Referee #1, 30 Jan 2021
Review of the paper:
“Investigating 3D and 4D Variational Rapid-Update-Cycling Assimilation of Weather Radar Reflectivity for a Flash Flood Event in Central Italy”
By: Vincenzo Mazzarella, Rossella Ferretti, Errico Picciotti, Frank S. Marzano
General comment
This paper shows the impact of 3D-Var/4D-Var cycling data assimilation of the WRF model for a case study occurred over central Italy in May 2018. CAPPI of radar reflectivity, provided by the Department of Civil Protection of Italy at 2, 3 and 5 km, are assimilated in WRF.
The Fraction Skill Score and the ROC curve and area are considered for the verification. Results show that the assimilation of radar reflectivity improves the precipitation forecast at 1h, 3h , 6h and 12h. Also, the 4DVar data assimilation shows better performance compared to 3DVar, especially considering the warm start.
While the paper is fluent and the subject interesting, there are major weaknesses that need to be addressed by the authors before this paper can be accepted for publication. In particular, there aren’t maps of forecasted precipitation and maps to understand, physically, which is the impact of the analysis on the background field.
Major points
- The introduction of the paper is poor and not representative of assimilation systems and weather forecasting models operating over Italy. A more complete review must be provided.
- Precipitation thresholds: The precipitation thresholds considered in sections 6.1.1 and 6.1.2 are small and not representative of heavy precipitation. The maximum intensity considered is 7 mm/1h, which is too small to be representative of a deep convective event.
- Precipitation fields: there are no model output of the precipitation. The only precipitation shown is the observed one. Precipitation forecast is discussed only using a statistical approach, without any example of what is predicted and how the rainfall forecast is improved by radar data assimilation. A map comparison of forecasted precipitation and observed precipitation must be provided in order to understand which is the impact of data assimilation for the case study.
- Analysis fields: we know that the CAPPIs of radar reflectivity are assimilated in WRF but we don’t know their effect. In general, when doing analyses, a comparison of the background and analysis fields must be shown to understand the impact of the data assimilation on the modeled fields. Nothing is shown.
Minor points
There are minor points to be considered. Please refer to the notes attached to pdf file to correct them.
-
AC1: 'Reply on RC1', Vincenzo Mazzarella, 30 Mar 2021
The comment was uploaded in the form of a supplement: https://nhess.copernicus.org/preprints/nhess-2020-406/nhess-2020-406-AC1-supplement.pdf
-
RC2: 'Comment on nhess-2020-406', Anonymous Referee #2, 02 Feb 2021
General comment
In this paper, the radar reflectivity measured by the Italian ground radar network is assimilated in the WRF model to simulate an event occurred on May 3, 2018 in central Italy. The impact of 3D and 4D variational rapid-update-cycling assimilation is compared with the control simulation using the Fraction Skill Score and the Receiver Operating Characteristic curve methods. Results show that the assimilation of radar reflectivity by 4DVar improves the precipitation forecast at 1h, 3h, 6h and 12h, especially considering the warm start.
While the precipitation forecast over the Mediterranean basin is very important, there are some key issues that need to be addressed by the authors before this paper can be accepted for publication.
Major points
- There is lack of the key figures to show the spatial results of 3DVar, 4DVar forecasting and control simulation in this paper.
- Figures (1-3) in this paper are in poor quality. It seems that they are not made by authors, just copied from some applications, there is no longitude or latitude in these figures at all. There are 9 plots in Figures 5-7 in same form, it is better to display them in one panel.
- The assimilation methods or evaluation methods are not novelty at all in this paper, it may be possible to show the efficient of forecasting. It is recommended to show the time cost and reasonable forecasting of 3DVar and 4DVar for 1day, 2days, 3days and even longer time, e.g. 7 days.
- This paper only shows the forecasting result of 1 day, it is far from the goal of forecasting for the Mediterranean basin, it is better to forecast for future 1 day, 2days, 3days and even longer time, e.g. 7 days.
- The 2×2 contingency tables and indicators such as POD, TS, FAR and ETS are recommended to evaluate the discrete variable, e.g. precipitation.
-
AC2: 'Reply on RC2', Vincenzo Mazzarella, 30 Mar 2021
The comment was uploaded in the form of a supplement: https://nhess.copernicus.org/preprints/nhess-2020-406/nhess-2020-406-AC2-supplement.pdf
Vincenzo Mazzarella et al.
Vincenzo Mazzarella et al.
Viewed
| HTML | XML | Total | BibTeX | EndNote | |
|---|---|---|---|---|---|
| 282 | 65 | 8 | 355 | 3 | 2 |
- HTML: 282
- PDF: 65
- XML: 8
- Total: 355
- BibTeX: 3
- EndNote: 2
Viewed (geographical distribution)
| Country | # | Views | % |
|---|
| Total: | 0 |
| HTML: | 0 |
| PDF: | 0 |
| XML: | 0 |
- 1