Full Text Available

Note: Clicking the button above will open the full text document at the original institutional repository in a new window.

Driving mechanisms of the Port Alfred upwelling cell inshore of the Agulhas Current

The presence of a semi-permanent upwelling cell, with a surface expression more than 40 % of the time has previously been described inshore of the Agulhas Current in the vicinity of Port Alfred, South Africa. This study employs a combination of in-situ mooring data, hydrographic cruises and satellit...

Full description

Saved in:
Bibliographic Details
Main Author: Malan, Neil
Other Authors: Ansorge, Isabelle Jane
Format: Thesis
Language:English
Published: Department of Oceanography 2014
Tags: Add Tag
No Tags, Be the first to tag this record!
_version_ 1867613214479482880
access_status_str Open Access
author Malan, Neil
author2 Ansorge, Isabelle Jane
author_browse Ansorge, Isabelle Jane
Malan, Neil
author_facet Ansorge, Isabelle Jane
Malan, Neil
author_sort Malan, Neil
collection Thesis
description The presence of a semi-permanent upwelling cell, with a surface expression more than 40 % of the time has previously been described inshore of the Agulhas Current in the vicinity of Port Alfred, South Africa. This study employs a combination of in-situ mooring data, hydrographic cruises and satellite remote sensing in order to investigate the nature and variability of this upwelling cell, as well as to investigate possible driving mechanisms. The study takes place over a period of 11 months. Special focus is given to the subsurface variability due to its possible implications for the greater Agulhas Bank environment. Upwelled water was found to be present on the shelf 85% of the time, highlighting the importance of subsurface variability in this area. The main timescales of variability were observed at 50-70 days, 8-12 days and 4-6 days. Upwelling was found to be maintained by continuous processes, driven by the interaction of the Agulhas Current with the changing bathymetry at Port Alfred. This upwelling is modulated by the effects of mesoscale features on the inshore edge of the current. While not a primary driver of upwelling, wind events were observed to have an effect on inshore bottom temperatures as well as the surface expression of the upwelling cell. A high degree of variability in was observed, with bottom temperatures at three mooring site fluctuating through a range of approximately 10° C. Future directions include further theoretical and idealised modeling studies to separate out the exact mechanisms of topographically driven, site-specific upwelling. The range of mesoscale interactions of the Agulhas Current with the shelf circulation also require further observational study.
format Thesis
id oai:open.uct.ac.za:11427/6676
institution University of Cape Town (South Africa)
language eng
last_indexed 2026-06-10T12:32:34.479Z
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:11427/6676 Driving mechanisms of the Port Alfred upwelling cell inshore of the Agulhas Current Malan, Neil Ansorge, Isabelle Jane Roberts, Mike The presence of a semi-permanent upwelling cell, with a surface expression more than 40 % of the time has previously been described inshore of the Agulhas Current in the vicinity of Port Alfred, South Africa. This study employs a combination of in-situ mooring data, hydrographic cruises and satellite remote sensing in order to investigate the nature and variability of this upwelling cell, as well as to investigate possible driving mechanisms. The study takes place over a period of 11 months. Special focus is given to the subsurface variability due to its possible implications for the greater Agulhas Bank environment. Upwelled water was found to be present on the shelf 85% of the time, highlighting the importance of subsurface variability in this area. The main timescales of variability were observed at 50-70 days, 8-12 days and 4-6 days. Upwelling was found to be maintained by continuous processes, driven by the interaction of the Agulhas Current with the changing bathymetry at Port Alfred. This upwelling is modulated by the effects of mesoscale features on the inshore edge of the current. While not a primary driver of upwelling, wind events were observed to have an effect on inshore bottom temperatures as well as the surface expression of the upwelling cell. A high degree of variability in was observed, with bottom temperatures at three mooring site fluctuating through a range of approximately 10° C. Future directions include further theoretical and idealised modeling studies to separate out the exact mechanisms of topographically driven, site-specific upwelling. The range of mesoscale interactions of the Agulhas Current with the shelf circulation also require further observational study. 2014-08-22T10:40:23Z 2014-08-22T10:40:23Z 2013 Master Thesis Masters MSc http://hdl.handle.net/11427/6676 eng application/pdf Department of Oceanography Faculty of Science University of Cape Town
spellingShingle Malan, Neil
Driving mechanisms of the Port Alfred upwelling cell inshore of the Agulhas Current
thesis_degree_str Master's
title Driving mechanisms of the Port Alfred upwelling cell inshore of the Agulhas Current
title_full Driving mechanisms of the Port Alfred upwelling cell inshore of the Agulhas Current
title_fullStr Driving mechanisms of the Port Alfred upwelling cell inshore of the Agulhas Current
title_full_unstemmed Driving mechanisms of the Port Alfred upwelling cell inshore of the Agulhas Current
title_short Driving mechanisms of the Port Alfred upwelling cell inshore of the Agulhas Current
title_sort driving mechanisms of the port alfred upwelling cell inshore of the agulhas current
url http://hdl.handle.net/11427/6676
work_keys_str_mv AT malanneil drivingmechanismsoftheportalfredupwellingcellinshoreoftheagulhascurrent