Interannual variability of rainfall in the Guinean Coast region and its links with sea surface temperature changes over the twentieth century for the different seasons
The summer Guinean Coast (GC) rainfall (GCR) displays a strong variability on different timescales that are driven by Sea Surface Temperature (SST) variations and amplified by land–atmosphere processes. However, the relationships between the GCR and SST modes of variability in the pre-monsoon (Mar...
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ftunistlouisbrus:oai:dial.uclouvain.be:boreal:236426 2024-05-12T08:08:14+00:00 Interannual variability of rainfall in the Guinean Coast region and its links with sea surface temperature changes over the twentieth century for the different seasons Worou, Koffi Goosse, Hugues Fichefet, Thierry Guichard, Françoise Diakhate, Moussa UCL - SST/ELI/ELIC - Earth & Climate 2020 http://hdl.handle.net/2078.1/236426 https://doi.org/10.1007/s00382-020-05276-5 eng eng boreal:236426 http://hdl.handle.net/2078.1/236426 doi:10.1007/s00382-020-05276-5 urn:ISSN:0930-7575 info:eu-repo/semantics/openAccess Climate Dynamics, Vol. 55, no.3-4, p. 449-470 (2020) Guinea Coast Rainfall Monsoon Teleconnection Variability Stationarity info:eu-repo/semantics/article 2020 ftunistlouisbrus https://doi.org/10.1007/s00382-020-05276-5 2024-04-18T17:21:38Z The summer Guinean Coast (GC) rainfall (GCR) displays a strong variability on different timescales that are driven by Sea Surface Temperature (SST) variations and amplified by land–atmosphere processes. However, the relationships between the GCR and SST modes of variability in the pre-monsoon (March–May, MAM), post-monsoon (October–November, ON) and Harmattan (December–February, DJF) seasons are not well known nor understood. Using observational dataset covering the twentieth century, we extend the conclusion obtained in previous studies that mainly analyzed the summer period (June–September, JJAS) by considering changes in SST-rainfall linkages throughout the year. We show that, in boreal winter, SST interannual variability in the tropical basins are anticorrelated with the GCR. The South Atlantic Ocean Dipole (SAOD) and the Atlantic Niño (ATL3) appear, however, as major drivers of the pre-monsoon and monsoon GCR. In MAM, both modes are in opposite phases with the GCR. Below normal SST in the tropical South Atlantic in MAM leads to a surface divergence south of the equator, and the resulting southerlies bring moist air into coastal Guinea, increasing rainfall. During JJAS, ATL3 and SAOD are in phase with the GCR. During ON, the eastern Mediterranean Sea anomalous warming strengthens the Saharan Heat Low, whose extension in the tropical North Atlantic enhances the low-level westerly Jet. This jet transports moisture into GC. The stationarity of the correlations between the GCR and SST indices has also been assessed, and the strongest and most stationary links are obtained during the monsoon season. Article in Journal/Newspaper North Atlantic South Atlantic Ocean DIAL@USL-B (Université Saint-Louis, Bruxelles) Climate Dynamics 55 3-4 449 470 |
institution |
Open Polar |
collection |
DIAL@USL-B (Université Saint-Louis, Bruxelles) |
op_collection_id |
ftunistlouisbrus |
language |
English |
topic |
Guinea Coast Rainfall Monsoon Teleconnection Variability Stationarity |
spellingShingle |
Guinea Coast Rainfall Monsoon Teleconnection Variability Stationarity Worou, Koffi Goosse, Hugues Fichefet, Thierry Guichard, Françoise Diakhate, Moussa Interannual variability of rainfall in the Guinean Coast region and its links with sea surface temperature changes over the twentieth century for the different seasons |
topic_facet |
Guinea Coast Rainfall Monsoon Teleconnection Variability Stationarity |
description |
The summer Guinean Coast (GC) rainfall (GCR) displays a strong variability on different timescales that are driven by Sea Surface Temperature (SST) variations and amplified by land–atmosphere processes. However, the relationships between the GCR and SST modes of variability in the pre-monsoon (March–May, MAM), post-monsoon (October–November, ON) and Harmattan (December–February, DJF) seasons are not well known nor understood. Using observational dataset covering the twentieth century, we extend the conclusion obtained in previous studies that mainly analyzed the summer period (June–September, JJAS) by considering changes in SST-rainfall linkages throughout the year. We show that, in boreal winter, SST interannual variability in the tropical basins are anticorrelated with the GCR. The South Atlantic Ocean Dipole (SAOD) and the Atlantic Niño (ATL3) appear, however, as major drivers of the pre-monsoon and monsoon GCR. In MAM, both modes are in opposite phases with the GCR. Below normal SST in the tropical South Atlantic in MAM leads to a surface divergence south of the equator, and the resulting southerlies bring moist air into coastal Guinea, increasing rainfall. During JJAS, ATL3 and SAOD are in phase with the GCR. During ON, the eastern Mediterranean Sea anomalous warming strengthens the Saharan Heat Low, whose extension in the tropical North Atlantic enhances the low-level westerly Jet. This jet transports moisture into GC. The stationarity of the correlations between the GCR and SST indices has also been assessed, and the strongest and most stationary links are obtained during the monsoon season. |
author2 |
UCL - SST/ELI/ELIC - Earth & Climate |
format |
Article in Journal/Newspaper |
author |
Worou, Koffi Goosse, Hugues Fichefet, Thierry Guichard, Françoise Diakhate, Moussa |
author_facet |
Worou, Koffi Goosse, Hugues Fichefet, Thierry Guichard, Françoise Diakhate, Moussa |
author_sort |
Worou, Koffi |
title |
Interannual variability of rainfall in the Guinean Coast region and its links with sea surface temperature changes over the twentieth century for the different seasons |
title_short |
Interannual variability of rainfall in the Guinean Coast region and its links with sea surface temperature changes over the twentieth century for the different seasons |
title_full |
Interannual variability of rainfall in the Guinean Coast region and its links with sea surface temperature changes over the twentieth century for the different seasons |
title_fullStr |
Interannual variability of rainfall in the Guinean Coast region and its links with sea surface temperature changes over the twentieth century for the different seasons |
title_full_unstemmed |
Interannual variability of rainfall in the Guinean Coast region and its links with sea surface temperature changes over the twentieth century for the different seasons |
title_sort |
interannual variability of rainfall in the guinean coast region and its links with sea surface temperature changes over the twentieth century for the different seasons |
publishDate |
2020 |
url |
http://hdl.handle.net/2078.1/236426 https://doi.org/10.1007/s00382-020-05276-5 |
genre |
North Atlantic South Atlantic Ocean |
genre_facet |
North Atlantic South Atlantic Ocean |
op_source |
Climate Dynamics, Vol. 55, no.3-4, p. 449-470 (2020) |
op_relation |
boreal:236426 http://hdl.handle.net/2078.1/236426 doi:10.1007/s00382-020-05276-5 urn:ISSN:0930-7575 |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1007/s00382-020-05276-5 |
container_title |
Climate Dynamics |
container_volume |
55 |
container_issue |
3-4 |
container_start_page |
449 |
op_container_end_page |
470 |
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1798851171007332352 |