Valley formation aridifies East Africa and elevates Congo Basin rainfall

East African aridification during the past 8 million years is frequently invoked as a driver of large-scale shifts in vegetation and the evolution of new animal lineages, including hominins. However, evidence for increasing aridity is debated5 and, crucially, the mechanisms leading to dry conditions...

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Váldodahkkit: Munday, C, Savage, N, Jones, RG, Washington, R
Materiálatiipa: Journal article
Giella:English
Almmustuhtton: Springer Nature 2023
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author Munday, C
Savage, N
Jones, RG
Washington, R
author_facet Munday, C
Savage, N
Jones, RG
Washington, R
author_sort Munday, C
collection OXFORD
description East African aridification during the past 8 million years is frequently invoked as a driver of large-scale shifts in vegetation and the evolution of new animal lineages, including hominins. However, evidence for increasing aridity is debated5 and, crucially, the mechanisms leading to dry conditions are unclear6. Here, numerical model experiments show that valleys punctuating the 6,000-km-long East African Rift System (EARS) are central to the development of dry conditions in East Africa. These valleys, including the Turkana Basin in Kenya, cause East Africa to dry by channelling water vapour towards Central Africa, a process that simultaneously enhances rainfall in the Congo Basin rainforest. Without the valleys, the uplift of the rift system leads to a wetter climate in East Africa and a drier climate in the Congo Basin. Results from climate model experiments demonstrate that the detailed tectonic development of Africa has shaped the rainfall distribution, with profound implications for the evolution of African plant and animal lineages.
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spelling oxford-uuid:f4365864-32fe-49d7-9344-4ab1b89d76de2024-12-04T11:05:59ZValley formation aridifies East Africa and elevates Congo Basin rainfallJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:f4365864-32fe-49d7-9344-4ab1b89d76deEnglishSymplectic ElementsSpringer Nature2023Munday, CSavage, NJones, RGWashington, REast African aridification during the past 8 million years is frequently invoked as a driver of large-scale shifts in vegetation and the evolution of new animal lineages, including hominins. However, evidence for increasing aridity is debated5 and, crucially, the mechanisms leading to dry conditions are unclear6. Here, numerical model experiments show that valleys punctuating the 6,000-km-long East African Rift System (EARS) are central to the development of dry conditions in East Africa. These valleys, including the Turkana Basin in Kenya, cause East Africa to dry by channelling water vapour towards Central Africa, a process that simultaneously enhances rainfall in the Congo Basin rainforest. Without the valleys, the uplift of the rift system leads to a wetter climate in East Africa and a drier climate in the Congo Basin. Results from climate model experiments demonstrate that the detailed tectonic development of Africa has shaped the rainfall distribution, with profound implications for the evolution of African plant and animal lineages.
spellingShingle Munday, C
Savage, N
Jones, RG
Washington, R
Valley formation aridifies East Africa and elevates Congo Basin rainfall
title Valley formation aridifies East Africa and elevates Congo Basin rainfall
title_full Valley formation aridifies East Africa and elevates Congo Basin rainfall
title_fullStr Valley formation aridifies East Africa and elevates Congo Basin rainfall
title_full_unstemmed Valley formation aridifies East Africa and elevates Congo Basin rainfall
title_short Valley formation aridifies East Africa and elevates Congo Basin rainfall
title_sort valley formation aridifies east africa and elevates congo basin rainfall
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AT savagen valleyformationaridifieseastafricaandelevatescongobasinrainfall
AT jonesrg valleyformationaridifieseastafricaandelevatescongobasinrainfall
AT washingtonr valleyformationaridifieseastafricaandelevatescongobasinrainfall