Constraining the exchange through the strait of Bab el Mandab

The strait of Bab el Mandab connects the Red Sea with the Indian ocean via the Gulf of Aden. The mean circulation at the strait is a three-layered exchange. The circulation in the Red Sea is understood to be driven by the air - sea fluxes, such as, evaporation and heat loss. We modify a thermohaline...

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Main Author: Satti, Samah Serelkhatem Abdelkareem
Format: Master Thesis
Language:English
Published: The University of Bergen 2012
Subjects:
Online Access:https://hdl.handle.net/1956/7077
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spelling ftunivbergen:oai:bora.uib.no:1956/7077 2023-05-15T15:03:02+02:00 Constraining the exchange through the strait of Bab el Mandab Satti, Samah Serelkhatem Abdelkareem 2012-10-01 930091 bytes application/pdf https://hdl.handle.net/1956/7077 eng eng The University of Bergen https://hdl.handle.net/1956/7077 Copyright the author. All rights reserved 756213 Master thesis 2012 ftunivbergen 2023-03-14T17:41:24Z The strait of Bab el Mandab connects the Red Sea with the Indian ocean via the Gulf of Aden. The mean circulation at the strait is a three-layered exchange. The circulation in the Red Sea is understood to be driven by the air - sea fluxes, such as, evaporation and heat loss. We modify a thermohaline circulation (THC) model originally developed for the Nordic Seas and Arctic Mediterranean by Eldevik and Nilsen (2010) to constrain the variability of THC at Bab el Mandab. We find that the surface and intermediate inflow branches are sensitive to change in heat and evaporation, but the deep outflow is predominantly sensitive to evap- oration only. The model suggests that the circulation is relatively sensitive to thermohaline change (about 17% - 44% of the mean flow). The model estimates a weaker thermohaline exchange at Bab el Mandab in 2050 using projected future climate change. Master i Meteorologi og oseanografi MAMN-GEOF GEOF399 Master Thesis Arctic Climate change Nordic Seas University of Bergen: Bergen Open Research Archive (BORA-UiB) Arctic Indian
institution Open Polar
collection University of Bergen: Bergen Open Research Archive (BORA-UiB)
op_collection_id ftunivbergen
language English
topic 756213
spellingShingle 756213
Satti, Samah Serelkhatem Abdelkareem
Constraining the exchange through the strait of Bab el Mandab
topic_facet 756213
description The strait of Bab el Mandab connects the Red Sea with the Indian ocean via the Gulf of Aden. The mean circulation at the strait is a three-layered exchange. The circulation in the Red Sea is understood to be driven by the air - sea fluxes, such as, evaporation and heat loss. We modify a thermohaline circulation (THC) model originally developed for the Nordic Seas and Arctic Mediterranean by Eldevik and Nilsen (2010) to constrain the variability of THC at Bab el Mandab. We find that the surface and intermediate inflow branches are sensitive to change in heat and evaporation, but the deep outflow is predominantly sensitive to evap- oration only. The model suggests that the circulation is relatively sensitive to thermohaline change (about 17% - 44% of the mean flow). The model estimates a weaker thermohaline exchange at Bab el Mandab in 2050 using projected future climate change. Master i Meteorologi og oseanografi MAMN-GEOF GEOF399
format Master Thesis
author Satti, Samah Serelkhatem Abdelkareem
author_facet Satti, Samah Serelkhatem Abdelkareem
author_sort Satti, Samah Serelkhatem Abdelkareem
title Constraining the exchange through the strait of Bab el Mandab
title_short Constraining the exchange through the strait of Bab el Mandab
title_full Constraining the exchange through the strait of Bab el Mandab
title_fullStr Constraining the exchange through the strait of Bab el Mandab
title_full_unstemmed Constraining the exchange through the strait of Bab el Mandab
title_sort constraining the exchange through the strait of bab el mandab
publisher The University of Bergen
publishDate 2012
url https://hdl.handle.net/1956/7077
geographic Arctic
Indian
geographic_facet Arctic
Indian
genre Arctic
Climate change
Nordic Seas
genre_facet Arctic
Climate change
Nordic Seas
op_relation https://hdl.handle.net/1956/7077
op_rights Copyright the author. All rights reserved
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