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Precipitation moisture sources of Ethiopian river basins and their role during drought conditions

Precipitation moisture sources of Ethiopian river basins and their role during drought conditions
Precipitation moisture sources of Ethiopian river basins and their role during drought conditions
In this study, we identified and investigated the annual climatological moisture sources for the Ethiopian river basins during 1980–2018. First, according to cluster analysis, the 12 river basins of this country were grouped into four regions: northeast (NE), southeast (SE), southwest (SW), and west (W), which were characterised by similar annual precipitation features. Global outputs from the Lagrangian FLEXPART model were used to investigate the air mass humidity gain before reaching each region. This revealed five main oceanic moisture sources located in the Mediterranean Sea, Red Sea, Indian Ocean, Persian Gulf, and the Arabian Sea, in addition to three main terrestrial moisture sources located in the African continent, Arabian Peninsula, and the regions themselves. Once the main climatological sources of moisture for each region were identified, a forward-in-time analysis of air masses over each source was performed to calculate the moisture contribution to precipitation E – P over the defined regions. The most important source at the annual scale for the NE, SW, and W regions is the African continent, while for the SE, it is the Indian Ocean. Indeed, terrestrial moisture sources are the major contributors to the precipitation over the NE, SW, and W, whereas oceanic sources are the major contributors to the SE. Another analysis identified the years affected by drought conditions in the regions. The role of the sources was evaluated for those years affected by severe and extreme drought, revealing the heterogeneous and also direct influences on the regions. Finally, according to the normalised difference vegetation index, the impacts of annual severe and extreme droughts were more prominent in areas of the NE and SE, but also in the SW during 1984.
Stojanovic, Milica
f8143b49-2387-4503-a223-c59306923b5e
Mulualem, Getachew Mehabie
88668cda-20ef-4543-a7e7-0a5f0c993d7b
Sorí, Rogert
1d467d75-d98a-4d0b-8ae9-b97716bdecc6
Vázquez, Marta
bee7de77-8c75-4530-8a02-a1300564f39b
Nieto, Raquel
4eaea1ca-c51f-4145-8479-28232c0cd636
Gimeno, Luis
6fb98c7b-93bc-477b-a8f0-188a0e04eac7
Stojanovic, Milica
f8143b49-2387-4503-a223-c59306923b5e
Mulualem, Getachew Mehabie
88668cda-20ef-4543-a7e7-0a5f0c993d7b
Sorí, Rogert
1d467d75-d98a-4d0b-8ae9-b97716bdecc6
Vázquez, Marta
bee7de77-8c75-4530-8a02-a1300564f39b
Nieto, Raquel
4eaea1ca-c51f-4145-8479-28232c0cd636
Gimeno, Luis
6fb98c7b-93bc-477b-a8f0-188a0e04eac7

Stojanovic, Milica, Mulualem, Getachew Mehabie, Sorí, Rogert, Vázquez, Marta, Nieto, Raquel and Gimeno, Luis (2022) Precipitation moisture sources of Ethiopian river basins and their role during drought conditions. Frontiers in Earth Science, 10, [929497]. (doi:10.3389/feart.2022.929497).

Record type: Article

Abstract

In this study, we identified and investigated the annual climatological moisture sources for the Ethiopian river basins during 1980–2018. First, according to cluster analysis, the 12 river basins of this country were grouped into four regions: northeast (NE), southeast (SE), southwest (SW), and west (W), which were characterised by similar annual precipitation features. Global outputs from the Lagrangian FLEXPART model were used to investigate the air mass humidity gain before reaching each region. This revealed five main oceanic moisture sources located in the Mediterranean Sea, Red Sea, Indian Ocean, Persian Gulf, and the Arabian Sea, in addition to three main terrestrial moisture sources located in the African continent, Arabian Peninsula, and the regions themselves. Once the main climatological sources of moisture for each region were identified, a forward-in-time analysis of air masses over each source was performed to calculate the moisture contribution to precipitation E – P over the defined regions. The most important source at the annual scale for the NE, SW, and W regions is the African continent, while for the SE, it is the Indian Ocean. Indeed, terrestrial moisture sources are the major contributors to the precipitation over the NE, SW, and W, whereas oceanic sources are the major contributors to the SE. Another analysis identified the years affected by drought conditions in the regions. The role of the sources was evaluated for those years affected by severe and extreme drought, revealing the heterogeneous and also direct influences on the regions. Finally, according to the normalised difference vegetation index, the impacts of annual severe and extreme droughts were more prominent in areas of the NE and SE, but also in the SW during 1984.

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Accepted/In Press date: 7 June 2022
Published date: 30 June 2022

Identifiers

Local EPrints ID: 507628
URI: http://eprints.soton.ac.uk/id/eprint/507628
PURE UUID: 34685a22-9c31-4ae9-8019-9dc1fbaee5bb
ORCID for Getachew Mehabie Mulualem: ORCID iD orcid.org/0000-0002-6488-4402

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Date deposited: 16 Dec 2025 17:33
Last modified: 18 Dec 2025 03:18

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Contributors

Author: Milica Stojanovic
Author: Getachew Mehabie Mulualem ORCID iD
Author: Rogert Sorí
Author: Marta Vázquez
Author: Raquel Nieto
Author: Luis Gimeno

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