Abstract
The yearly exceedance probability of extreme precipitation of multiple durations is crucial for infrastructure design, risk management, and policymaking. Local extremes emerge from the interaction of weather systems with local terrain features such as coastlines and orography; however, multi-duration extremes do not follow exactly the patterns of cumulative precipitation and are still not well understood. High-resolution information from weather radars could help us quantify their patterns better, but traditional extreme value analyses based on radar records were found to be too inaccurate for quantifying the extreme intensities required for impact studies. Here, we propose a novel methodology for extreme precipitation frequency analysis based on relatively short weather radar records, and we use it to investigate the coastal and orographic effects on extreme precipitation of durations between 10g min and 24g h. Combining 11 years of radar data with 10g min rain gauge data in the southeastern Mediterranean, we obtain estimates of the once in 100 years precipitation intensities with g1/426g % standard error, which is lower than those obtained using traditional approaches on rain gauge data. We identify the following three distinct regimes which respond differently to coastal and orographic forcing: short durations (g1/410g min), related to peak convective rain rates, hourly durations (g1/41g h), related to the yield of individual convective cells, and long durations (g1/46-24g h), related to the accumulation of multiple convective cells and to stratiform processes. At short and hourly durations, extreme return levels peak at the coastline, while at longer durations they peak corresponding to the orographic barriers. The distributions tail heaviness is rather uniform above the sea and rapidly changes in presence of orography, with opposing directions at short (decreasing tail heaviness, with a peak at hourly durations) and long (increasing) durations. These distinct effects suggest that short-scale hazards, such as urban pluvial floods, could be more of concern for the coastal regions, while longer-scale hazards, such as flash floods, could be more relevant in mountainous areas.
Original language | American English |
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Pages (from-to) | 1439-1458 |
Number of pages | 20 |
Journal | Hydrology and Earth System Sciences |
Volume | 26 |
Issue number | 5 |
DOIs | |
State | Published - 15 Mar 2022 |
Bibliographical note
Funding Information:This study is a contribution to the HyMeX program, and is based upon work from COST Action CA19109 “MedCyclones” supported by COST – European Cooperation in Science and Technology. Francesco Marra thanks the Institute of Atmospheric Sciences and Climate (ISAC) of the National Research Council of Italy (CNR) for the support. Moshe Armon was supported by an ETH Zurich Postdoctoral Fellowship (project no. 21-1 FEL-67), by the Stiftung fuer naturwissenschaftliche und technische Forschung, and the ETH Zurich Foundation. The authors thank Uri Dayan, for the fruitful discussions, and the two reviewers, for the constructive comments.
Funding Information:
This paper collects years of efforts. Many of the methods used to create the weather radar archive were developed by the team in the past years, in addition to the novel statistical methodology used for extreme value analyses. Similarly, studies about extreme precipitation in the region and about the use of remotely sensed datasets for precipitation frequency analyses were published by the team. The number of self-citations is, thus, large. We did our best not to inflate it, and we hope the text will clarify why these citations are needed. This study is a contribution to the HyMeX program, and is based upon work from COST Action CA19109 "MedCyclones" supported by COST ? European Cooperation in Science and Technology. Francesco Marra thanks the Institute of Atmospheric Sciences and Climate (ISAC) of the National Research Council of Italy (CNR) for the support. Moshe Armon was supported by an ETH Zurich Postdoctoral Fellowship (project no. 21-1 FEL-67), by the Stiftung fuer naturwissenschaftliche und technische Forschung, and the ETH Zurich Foundation. The authors thank Uri Dayan, for the fruitful discussions, and the two reviewers, for the constructive comments. This research has been supported by the Israel Science Foundation (grant no.?1069/18).
Funding Information:
Financial support. This research has been supported by the Israel
Publisher Copyright:
© 2022 Francesco Marra et al.