African low‐level jets and their importance for water vapor transport and rainfall

Uncertainty in the future evolution of tropical rainfall is linked to circulation changes under warming. In Africa, a key barrier to interpreting rainfall changes is our limited understanding of water vapor transport across the continent. Here, we show that a series of nocturnal easterly Low-Level J...

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Main Authors: Munday, C, Washington, R, Hart, N
Format: Journal article
Language:English
Published: AGU 2020
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author Munday, C
Washington, R
Hart, N
author_facet Munday, C
Washington, R
Hart, N
author_sort Munday, C
collection OXFORD
description Uncertainty in the future evolution of tropical rainfall is linked to circulation changes under warming. In Africa, a key barrier to interpreting rainfall changes is our limited understanding of water vapor transport across the continent. Here, we show that a series of nocturnal easterly Low-Level Jets (LLJs), which form in the valleys punctuating the East African rift system, transport the majority of water vapor to central Africa from the Indian Ocean. There is a robust connection between strengthened LLJs and drought in eastern and southern Africa at interannual timescales, mediated by an increase in low-level divergence and water vapor export. Analysis of climate model simulations at a wide range of resolutions (250–4.5 km) suggests that grid lengths <60 km are needed to simulate the salient structures of LLJs. The failure of coarse resolution models to capture LLJs is linked with biases in rainfall climatology and variability across the continent.
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spelling oxford-uuid:4fbaba19-3d02-4392-a6cd-9815021a50aa2024-11-22T18:32:03ZAfrican low‐level jets and their importance for water vapor transport and rainfallJournal articlehttp://purl.org/coar/resource_type/c_545buuid:4fbaba19-3d02-4392-a6cd-9815021a50aaEnglishBulkUploadREACH articlesAGU2020Munday, CWashington, RHart, NUncertainty in the future evolution of tropical rainfall is linked to circulation changes under warming. In Africa, a key barrier to interpreting rainfall changes is our limited understanding of water vapor transport across the continent. Here, we show that a series of nocturnal easterly Low-Level Jets (LLJs), which form in the valleys punctuating the East African rift system, transport the majority of water vapor to central Africa from the Indian Ocean. There is a robust connection between strengthened LLJs and drought in eastern and southern Africa at interannual timescales, mediated by an increase in low-level divergence and water vapor export. Analysis of climate model simulations at a wide range of resolutions (250–4.5 km) suggests that grid lengths <60 km are needed to simulate the salient structures of LLJs. The failure of coarse resolution models to capture LLJs is linked with biases in rainfall climatology and variability across the continent.
spellingShingle Munday, C
Washington, R
Hart, N
African low‐level jets and their importance for water vapor transport and rainfall
title African low‐level jets and their importance for water vapor transport and rainfall
title_full African low‐level jets and their importance for water vapor transport and rainfall
title_fullStr African low‐level jets and their importance for water vapor transport and rainfall
title_full_unstemmed African low‐level jets and their importance for water vapor transport and rainfall
title_short African low‐level jets and their importance for water vapor transport and rainfall
title_sort african low level jets and their importance for water vapor transport and rainfall
work_keys_str_mv AT mundayc africanlowleveljetsandtheirimportanceforwatervaportransportandrainfall
AT washingtonr africanlowleveljetsandtheirimportanceforwatervaportransportandrainfall
AT hartn africanlowleveljetsandtheirimportanceforwatervaportransportandrainfall