Relationship of Sahel Precipitation and Atmospheric Centers of Action
The dynamics associated with drought in the Sahel have attracted considerable attention in the recent literature. This paper evaluates Sahel precipitation using the paradigm of the atmospheric centers of action, that is, the extended semipermanent highs and lows that dominate regional circulations a...
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2012-01-01
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Series: | Advances in Meteorology |
Online Access: | http://dx.doi.org/10.1155/2012/953853 |
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doaj-7986b805876443f895d4c508886007b42020-11-24T23:28:24ZengHindawi LimitedAdvances in Meteorology1687-93091687-93172012-01-01201210.1155/2012/953853953853Relationship of Sahel Precipitation and Atmospheric Centers of ActionSultan Hameed0Nicole Riemer1School for Marine and Atmospheric Sciences, Stony Brook University, Stony Brook, NY 11794-5000, USADepartment of Atmospheric Sciences, University of Illinois, Urbana, IL 61801, USAThe dynamics associated with drought in the Sahel have attracted considerable attention in the recent literature. This paper evaluates Sahel precipitation using the paradigm of the atmospheric centers of action, that is, the extended semipermanent highs and lows that dominate regional circulations and are evident in sea level pressure patterns. We find that Sahel precipitation is significantly influenced by changes in the Azores High and the South Asia Low. Specifically, about 50 percent of the variance of July to September rainfall over the Sahel is explained by changes in the Azores High Longitude position and South Asia Low pressure. In contrast, the contribution of the Southern Oscillation to Sahel precipitation is smaller in comparison. Results presented in this paper suggest that a key test for a climate model in simulating variability of Sahel rainfall is the accuracy with which the model simulates the dynamics of South Asia Low and the Azores High.http://dx.doi.org/10.1155/2012/953853 |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Sultan Hameed Nicole Riemer |
spellingShingle |
Sultan Hameed Nicole Riemer Relationship of Sahel Precipitation and Atmospheric Centers of Action Advances in Meteorology |
author_facet |
Sultan Hameed Nicole Riemer |
author_sort |
Sultan Hameed |
title |
Relationship of Sahel Precipitation and Atmospheric Centers of Action |
title_short |
Relationship of Sahel Precipitation and Atmospheric Centers of Action |
title_full |
Relationship of Sahel Precipitation and Atmospheric Centers of Action |
title_fullStr |
Relationship of Sahel Precipitation and Atmospheric Centers of Action |
title_full_unstemmed |
Relationship of Sahel Precipitation and Atmospheric Centers of Action |
title_sort |
relationship of sahel precipitation and atmospheric centers of action |
publisher |
Hindawi Limited |
series |
Advances in Meteorology |
issn |
1687-9309 1687-9317 |
publishDate |
2012-01-01 |
description |
The dynamics associated with drought in the Sahel have attracted considerable attention in the recent literature. This paper evaluates Sahel precipitation using the paradigm of the atmospheric centers of action, that is, the extended semipermanent highs and lows that dominate regional circulations and are evident in sea level pressure patterns. We find that Sahel precipitation is significantly influenced by changes in the Azores High and the South Asia Low. Specifically, about 50 percent of the variance of July to September rainfall over the Sahel is explained by changes in the Azores High Longitude position and South Asia Low pressure. In contrast, the contribution of the Southern Oscillation to Sahel precipitation is smaller in comparison. Results presented in this paper suggest that a key test for a climate model in simulating variability of Sahel rainfall is the accuracy with which the model simulates the dynamics of South Asia Low and the Azores High. |
url |
http://dx.doi.org/10.1155/2012/953853 |
work_keys_str_mv |
AT sultanhameed relationshipofsahelprecipitationandatmosphericcentersofaction AT nicoleriemer relationshipofsahelprecipitationandatmosphericcentersofaction |
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1725549279793119232 |