Small scale thermohaline ocean circulation

Master's thesis in Petroleum engineering Upon examining the how convective flows are generated in the ocean, Henry Stommel presented a simple idealized model called the Stommel model (1961) to better understand how salinity and temperature differences can affect the ocean circulation between th...

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Main Author: Wanyenze, Joan Shanita
Other Authors: Rabenjafimanantsoa, A.H., Skadsem, Hans Joakim, Time, Rune Wiggo
Format: Master Thesis
Language:English
Published: University of Stavanger, Norway 2020
Subjects:
Online Access:https://hdl.handle.net/11250/2685491
id ftunivstavanger:oai:uis.brage.unit.no:11250/2685491
record_format openpolar
spelling ftunivstavanger:oai:uis.brage.unit.no:11250/2685491 2023-06-11T04:09:07+02:00 Small scale thermohaline ocean circulation Wanyenze, Joan Shanita Rabenjafimanantsoa, A.H. Skadsem, Hans Joakim Time, Rune Wiggo 2020-07-15 application/pdf https://hdl.handle.net/11250/2685491 eng eng University of Stavanger, Norway Masteroppgave/UIS-TN-IEP/2020; https://hdl.handle.net/11250/2685491 Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no petroleumsteknologi petroleum engineering Stommel model thermohaline circulation ocean circulation overturn circulation freshwater input VDP::Teknologi: 500::Berg‑ og petroleumsfag: 510::Petroleumsteknologi: 512 Master thesis 2020 ftunivstavanger 2023-05-29T16:04:13Z Master's thesis in Petroleum engineering Upon examining the how convective flows are generated in the ocean, Henry Stommel presented a simple idealized model called the Stommel model (1961) to better understand how salinity and temperature differences can affect the ocean circulation between the Arctic and Atlantic. The ocean circulation is named thermohaline circulation. This thesis implements the Stommel model using a small scale setup filled with a salt mixture including external systems duplicating the Arctic and Atlantic like the buffer system and evaporation system respectively. A mass balance of the salt content is to preserved throughout the experiment, however it was observed that this was not the case. Despite some mishaps in the data collection, measurements of the conductivity show lessened value in both basins plus a salt accumulation in the evaporation system meaning an ineffective salt drive to the Atlantic basin. It was also observed that the freshwater input reached a maximum limit and transitions between the circulation modes were abrupt. Suggestions to modifications in terms of the setup were discussed, however these have some limitations. Nonetheless, this thesis can be used a precursor to see how complex and diverse the thermohaline circulation really is. Master Thesis Arctic University of Stavanger: UiS Brage Arctic
institution Open Polar
collection University of Stavanger: UiS Brage
op_collection_id ftunivstavanger
language English
topic petroleumsteknologi
petroleum engineering
Stommel model
thermohaline circulation
ocean circulation
overturn circulation
freshwater input
VDP::Teknologi: 500::Berg‑ og petroleumsfag: 510::Petroleumsteknologi: 512
spellingShingle petroleumsteknologi
petroleum engineering
Stommel model
thermohaline circulation
ocean circulation
overturn circulation
freshwater input
VDP::Teknologi: 500::Berg‑ og petroleumsfag: 510::Petroleumsteknologi: 512
Wanyenze, Joan Shanita
Small scale thermohaline ocean circulation
topic_facet petroleumsteknologi
petroleum engineering
Stommel model
thermohaline circulation
ocean circulation
overturn circulation
freshwater input
VDP::Teknologi: 500::Berg‑ og petroleumsfag: 510::Petroleumsteknologi: 512
description Master's thesis in Petroleum engineering Upon examining the how convective flows are generated in the ocean, Henry Stommel presented a simple idealized model called the Stommel model (1961) to better understand how salinity and temperature differences can affect the ocean circulation between the Arctic and Atlantic. The ocean circulation is named thermohaline circulation. This thesis implements the Stommel model using a small scale setup filled with a salt mixture including external systems duplicating the Arctic and Atlantic like the buffer system and evaporation system respectively. A mass balance of the salt content is to preserved throughout the experiment, however it was observed that this was not the case. Despite some mishaps in the data collection, measurements of the conductivity show lessened value in both basins plus a salt accumulation in the evaporation system meaning an ineffective salt drive to the Atlantic basin. It was also observed that the freshwater input reached a maximum limit and transitions between the circulation modes were abrupt. Suggestions to modifications in terms of the setup were discussed, however these have some limitations. Nonetheless, this thesis can be used a precursor to see how complex and diverse the thermohaline circulation really is.
author2 Rabenjafimanantsoa, A.H.
Skadsem, Hans Joakim
Time, Rune Wiggo
format Master Thesis
author Wanyenze, Joan Shanita
author_facet Wanyenze, Joan Shanita
author_sort Wanyenze, Joan Shanita
title Small scale thermohaline ocean circulation
title_short Small scale thermohaline ocean circulation
title_full Small scale thermohaline ocean circulation
title_fullStr Small scale thermohaline ocean circulation
title_full_unstemmed Small scale thermohaline ocean circulation
title_sort small scale thermohaline ocean circulation
publisher University of Stavanger, Norway
publishDate 2020
url https://hdl.handle.net/11250/2685491
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_relation Masteroppgave/UIS-TN-IEP/2020;
https://hdl.handle.net/11250/2685491
op_rights Navngivelse 4.0 Internasjonal
http://creativecommons.org/licenses/by/4.0/deed.no
_version_ 1768382839953293312