The missing teleconnection between the North Atlantic and the Sahel precipitation in CFSv2
Abstract This study presents new findings on the link between interannual variabilities of atmospheric circulations over the North Atlantic and precipitation over the African Sahel ( P S ). Our analysis shows a meridionally stratified circulation wave train resembling the East Atlantic ( EA ) mode,...
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crwiley:10.1002/asl2.457 2024-06-02T08:11:01+00:00 The missing teleconnection between the North Atlantic and the Sahel precipitation in CFSv2 Barandiaran, Daniel Wang, Shih‐Yu 2013 http://dx.doi.org/10.1002/asl2.457 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fasl2.457 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/asl2.457 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Atmospheric Science Letters volume 15, issue 1, page 21-28 ISSN 1530-261X 1530-261X journal-article 2013 crwiley https://doi.org/10.1002/asl2.457 2024-05-03T10:41:00Z Abstract This study presents new findings on the link between interannual variabilities of atmospheric circulations over the North Atlantic and precipitation over the African Sahel ( P S ). Our analysis shows a meridionally stratified circulation wave train resembling the East Atlantic ( EA ) mode, apparently connected to P S through Rossby wave dispersion in the middle troposphere originating from the North Atlantic. However, the Climate Forecast System version 2 fails to depict the EA and its P S impact. Because the EA explains 29% of variance of P S , this portion of P S variability is either missing in the seasonal forecast, or being made up by an alternative process . Article in Journal/Newspaper North Atlantic Wiley Online Library Atmospheric Science Letters 15 1 21 28 |
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Wiley Online Library |
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English |
description |
Abstract This study presents new findings on the link between interannual variabilities of atmospheric circulations over the North Atlantic and precipitation over the African Sahel ( P S ). Our analysis shows a meridionally stratified circulation wave train resembling the East Atlantic ( EA ) mode, apparently connected to P S through Rossby wave dispersion in the middle troposphere originating from the North Atlantic. However, the Climate Forecast System version 2 fails to depict the EA and its P S impact. Because the EA explains 29% of variance of P S , this portion of P S variability is either missing in the seasonal forecast, or being made up by an alternative process . |
format |
Article in Journal/Newspaper |
author |
Barandiaran, Daniel Wang, Shih‐Yu |
spellingShingle |
Barandiaran, Daniel Wang, Shih‐Yu The missing teleconnection between the North Atlantic and the Sahel precipitation in CFSv2 |
author_facet |
Barandiaran, Daniel Wang, Shih‐Yu |
author_sort |
Barandiaran, Daniel |
title |
The missing teleconnection between the North Atlantic and the Sahel precipitation in CFSv2 |
title_short |
The missing teleconnection between the North Atlantic and the Sahel precipitation in CFSv2 |
title_full |
The missing teleconnection between the North Atlantic and the Sahel precipitation in CFSv2 |
title_fullStr |
The missing teleconnection between the North Atlantic and the Sahel precipitation in CFSv2 |
title_full_unstemmed |
The missing teleconnection between the North Atlantic and the Sahel precipitation in CFSv2 |
title_sort |
missing teleconnection between the north atlantic and the sahel precipitation in cfsv2 |
publisher |
Wiley |
publishDate |
2013 |
url |
http://dx.doi.org/10.1002/asl2.457 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fasl2.457 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/asl2.457 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Atmospheric Science Letters volume 15, issue 1, page 21-28 ISSN 1530-261X 1530-261X |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/asl2.457 |
container_title |
Atmospheric Science Letters |
container_volume |
15 |
container_issue |
1 |
container_start_page |
21 |
op_container_end_page |
28 |
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1800757018830569472 |