Future intensification of precipitation and wind gust associated thunderstorms over Lake Victoria

Severe thunderstorms affect more than 30 million people living along the shores of Lake Victoria (East Africa). Thousands of fishers lose their lives on the lake every year. While deadly waves are assumed to be initiated by severe wind gusts, knowledge about thunderstorms is restricted to precipitat...

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Autores principales: Jonas Van de Walle, Wim Thiery, Roman Brogli, Olivia Martius, Jakob Zscheischler, Nicole P.M. van Lipzig
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Lenguaje:EN
Publicado: Elsevier 2021
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Acceso en línea:https://doaj.org/article/500c36ff8ce049b8b1f97c5e5a053d38
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spelling oai:doaj.org-article:500c36ff8ce049b8b1f97c5e5a053d382021-11-10T04:25:19ZFuture intensification of precipitation and wind gust associated thunderstorms over Lake Victoria2212-094710.1016/j.wace.2021.100391https://doaj.org/article/500c36ff8ce049b8b1f97c5e5a053d382021-12-01T00:00:00Zhttp://www.sciencedirect.com/science/article/pii/S2212094721000803https://doaj.org/toc/2212-0947Severe thunderstorms affect more than 30 million people living along the shores of Lake Victoria (East Africa). Thousands of fishers lose their lives on the lake every year. While deadly waves are assumed to be initiated by severe wind gusts, knowledge about thunderstorms is restricted to precipitation or environmental proxies. Here we use a regional climate model run at convection-permitting resolution to simulate both precipitation and wind gusts over Lake Victoria for a historical 10-year period. In addition, a pseudo global warming simulation provides insight into the region’s future climate. In this simulation, ERA5’s initial and boundary conditions are perturbed with atmospheric changes between 1995–2025 and 2070–2100, projected by CMIP6’s ensemble mean. It was found that future decreases in both mean precipitation and wind gusts over Lake Victoria can be attributed to a weaker mean mesoscale circulation that reduces the trigger for over-lake nighttime convection and decreases the mean wind shear. However, an intensification of extremes is projected for both over-lake precipitation and wind gusts. The observed ∼7 %K−1 Clausius–Clapeyron extreme precipitation scaling is ascribed to increased water vapor content and a compensation of weaker mesoscale circulations and stronger thunderstorm dynamics. More frequent wind gust extremes result from higher wind shear conditions and more compound thunderstorms with both intense rainfall and severe wind gusts. Overall, our study emphasizes Lake Victoria’s modulating role in determining regional current and future extremes, in addition to changes expected from the Clausius–Clapeyron relation.Jonas Van de WalleWim ThieryRoman BrogliOlivia MartiusJakob ZscheischlerNicole P.M. van LipzigElsevierarticleLake VictoriaRegional climate modelingClimate projectionsSevere wind gustsIntense precipitationCompound eventsMeteorology. ClimatologyQC851-999ENWeather and Climate Extremes, Vol 34, Iss , Pp 100391- (2021)
institution DOAJ
collection DOAJ
language EN
topic Lake Victoria
Regional climate modeling
Climate projections
Severe wind gusts
Intense precipitation
Compound events
Meteorology. Climatology
QC851-999
spellingShingle Lake Victoria
Regional climate modeling
Climate projections
Severe wind gusts
Intense precipitation
Compound events
Meteorology. Climatology
QC851-999
Jonas Van de Walle
Wim Thiery
Roman Brogli
Olivia Martius
Jakob Zscheischler
Nicole P.M. van Lipzig
Future intensification of precipitation and wind gust associated thunderstorms over Lake Victoria
description Severe thunderstorms affect more than 30 million people living along the shores of Lake Victoria (East Africa). Thousands of fishers lose their lives on the lake every year. While deadly waves are assumed to be initiated by severe wind gusts, knowledge about thunderstorms is restricted to precipitation or environmental proxies. Here we use a regional climate model run at convection-permitting resolution to simulate both precipitation and wind gusts over Lake Victoria for a historical 10-year period. In addition, a pseudo global warming simulation provides insight into the region’s future climate. In this simulation, ERA5’s initial and boundary conditions are perturbed with atmospheric changes between 1995–2025 and 2070–2100, projected by CMIP6’s ensemble mean. It was found that future decreases in both mean precipitation and wind gusts over Lake Victoria can be attributed to a weaker mean mesoscale circulation that reduces the trigger for over-lake nighttime convection and decreases the mean wind shear. However, an intensification of extremes is projected for both over-lake precipitation and wind gusts. The observed ∼7 %K−1 Clausius–Clapeyron extreme precipitation scaling is ascribed to increased water vapor content and a compensation of weaker mesoscale circulations and stronger thunderstorm dynamics. More frequent wind gust extremes result from higher wind shear conditions and more compound thunderstorms with both intense rainfall and severe wind gusts. Overall, our study emphasizes Lake Victoria’s modulating role in determining regional current and future extremes, in addition to changes expected from the Clausius–Clapeyron relation.
format article
author Jonas Van de Walle
Wim Thiery
Roman Brogli
Olivia Martius
Jakob Zscheischler
Nicole P.M. van Lipzig
author_facet Jonas Van de Walle
Wim Thiery
Roman Brogli
Olivia Martius
Jakob Zscheischler
Nicole P.M. van Lipzig
author_sort Jonas Van de Walle
title Future intensification of precipitation and wind gust associated thunderstorms over Lake Victoria
title_short Future intensification of precipitation and wind gust associated thunderstorms over Lake Victoria
title_full Future intensification of precipitation and wind gust associated thunderstorms over Lake Victoria
title_fullStr Future intensification of precipitation and wind gust associated thunderstorms over Lake Victoria
title_full_unstemmed Future intensification of precipitation and wind gust associated thunderstorms over Lake Victoria
title_sort future intensification of precipitation and wind gust associated thunderstorms over lake victoria
publisher Elsevier
publishDate 2021
url https://doaj.org/article/500c36ff8ce049b8b1f97c5e5a053d38
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AT wimthiery futureintensificationofprecipitationandwindgustassociatedthunderstormsoverlakevictoria
AT romanbrogli futureintensificationofprecipitationandwindgustassociatedthunderstormsoverlakevictoria
AT oliviamartius futureintensificationofprecipitationandwindgustassociatedthunderstormsoverlakevictoria
AT jakobzscheischler futureintensificationofprecipitationandwindgustassociatedthunderstormsoverlakevictoria
AT nicolepmvanlipzig futureintensificationofprecipitationandwindgustassociatedthunderstormsoverlakevictoria
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