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Water vapour transport from the South Atlantic and Indian Oceans and summer rainfall in southern Africa

Includes bibliographical references (p. 190-206).

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Bibliographic Details
Main Author: Vigaud, Nicolas
Other Authors: Rouault, Mathieu
Format: Thesis
Language:English
Published: Department of Oceanography 2014
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access_status_str Open Access
author Vigaud, Nicolas
author2 Rouault, Mathieu
author_browse Rouault, Mathieu
Vigaud, Nicolas
author_facet Rouault, Mathieu
Vigaud, Nicolas
author_sort Vigaud, Nicolas
collection Thesis
description Includes bibliographical references (p. 190-206).
format Thesis
id oai:open.uct.ac.za:11427/6447
institution University of Cape Town (South Africa)
language eng
last_indexed 2026-06-10T12:32:00.945Z
license_str Not specified — see source repository
provenance_str_mv Harvested via OAI-PMH from UCTD — University of Cape Town Open Access Repository
publishDate 2014
publishDateRange 2014
publishDateSort 2014
publisher Department of Oceanography
publisherStr Department of Oceanography
record_format dspace
source_str UCTD — University of Cape Town Open Access Repository
spelling oai:open.uct.ac.za:11427/6447 Water vapour transport from the South Atlantic and Indian Oceans and summer rainfall in southern Africa Vigaud, Nicolas Rouault, Mathieu Oceanography Includes bibliographical references (p. 190-206). Moisture input from the South Atlantic and Indian Oceans over southern Africa is examined through zonal water vapour transport. Along the west coast, variations in intensity and latitudinal position of the South Atlantic anticyclone/modulations of the westerly flow that penetrates from the tropical Atlantic, contribute the most about 25% and 11% of the variance explained respectively), in January-February to variability in moisture advection from the South/tropical Atlantic, thus affecting rainfall at subtropical/tropical latitudes respectively. The southern extension of the AEJ could play a role in transfering moisture from the tropics southwards during wet phases, while events related to low phases of the Southern Oscillation are marked by an eastward shift of the ascending branch of the Walker circulation, suppressing convection and thus reducing rainfall over the subcontinent. 2014-08-13T19:44:23Z 2014-08-13T19:44:23Z 2007 Doctoral Thesis Doctoral PhD http://hdl.handle.net/11427/6447 eng application/pdf Department of Oceanography Faculty of Science University of Cape Town
spellingShingle Oceanography
Vigaud, Nicolas
Water vapour transport from the South Atlantic and Indian Oceans and summer rainfall in southern Africa
thesis_degree_str Doctoral
title Water vapour transport from the South Atlantic and Indian Oceans and summer rainfall in southern Africa
title_full Water vapour transport from the South Atlantic and Indian Oceans and summer rainfall in southern Africa
title_fullStr Water vapour transport from the South Atlantic and Indian Oceans and summer rainfall in southern Africa
title_full_unstemmed Water vapour transport from the South Atlantic and Indian Oceans and summer rainfall in southern Africa
title_short Water vapour transport from the South Atlantic and Indian Oceans and summer rainfall in southern Africa
title_sort water vapour transport from the south atlantic and indian oceans and summer rainfall in southern africa
topic Oceanography
url http://hdl.handle.net/11427/6447
work_keys_str_mv AT vigaudnicolas watervapourtransportfromthesouthatlanticandindianoceansandsummerrainfallinsouthernafrica