Numerical Simulation of Sediment Transport at the Agulhas Drift on the South African Gateway in relation to its Geodynamic Development
The South African Gateway is a critical region for the water mass exchange between the Atlantic and the Indian Ocean. The variability in the interoceanic exchange is relevant to global climate change. High resolution seismic reflection data were collected in the Transkei Basin during R/V SONNE cruis...
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Universität Bremen
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ftsubbremen:oai:media.suub.uni-bremen.de:Publications/elib/282 2023-05-15T14:04:15+02:00 Numerical Simulation of Sediment Transport at the Agulhas Drift on the South African Gateway in relation to its Geodynamic Development Numerische Simulation von Sediment-Transport im Gebiet der Agulhas-Drift am Südafrikanischen Tor in Bezug auf die geodynamische Entwicklung Li, Xin Miller, Heinrich Huhn, Katrin 2012-02-09 application/pdf https://media.suub.uni-bremen.de/handle/elib/282 https://nbn-resolving.org/urn:nbn:de:gbv:46-00102528-18 eng eng Universität Bremen FB5 Geowissenschaften https://media.suub.uni-bremen.de/handle/elib/282 urn:nbn:de:gbv:46-00102528-18 info:eu-repo/semantics/openAccess Numerical model Sediment transport silt Agulhas Drift Agulhas Plateau Transkei Basin South African Gateway Regional Oceanic Modeling System ROMS Antarctic Bottom Water AABW North Atlantic Deep Water NADW eddy eddy kinetic energy EKE 550 550 Earth sciences and geology ddc:550 Dissertation doctoralThesis 2012 ftsubbremen 2022-11-09T07:09:20Z The South African Gateway is a critical region for the water mass exchange between the Atlantic and the Indian Ocean. The variability in the interoceanic exchange is relevant to global climate change. High resolution seismic reflection data were collected in the Transkei Basin during R/V SONNE cruise SO 182 in 2005. These seismic observations have indicated that a large elongate mounded contourite drift, the Agulhas Drift, has been built up by eastward flows of Antarctic Bottom Water (AABW) and North Atlantic Deep Water (NADW) since about 3 Ma. For a better understanding of the influences of the various currents on sediment transport patterns in the vicinity of the Agulhas Drift, the Regional Oceanic Modeling System (ROMS) has been used to simulate the current system and suspended sediment transport processes. The results from current system simulation showed that a recurrent individual cyclonic eddy event is the key hydrodynamic feature in the Transkei Basin. These eddies are almost fixed in the center of the Transkei Basin and spread over the entire water column. Flow in their northern segments is eastward across the southern flank of the Agulhas Drift. These eddies are supposedly the result of perturbations in the Subtropical Convergence (STC) in the region of south of Africa, where planetary waves on the STC deform. The perturbations enhance the surface eddy kinetic energy (EKE) in the Transkei Basin. The high EKE is then transferred from the surface to the deep ocean, where it causes the formation of eddies at abyssal depth. Based on the ocean circulation simulations, grain size experiments were carried out to test the transport behaviors for 4 different silt grain size classes. Our simulations reveal that sediment transport patterns in the Transkei Basin are strongly influenced by the mesoscale eddies. During eddy events, silts at all tested grain sizes can be resuspended by the AABW along the northeastern flank of the Agulhas Plateau that borders the Transkei Bsin to the east, whereas not all of them can ... Doctoral or Postdoctoral Thesis Antarc* Antarctic NADW North Atlantic Deep Water North Atlantic Media SuUB Bremen (Staats- und Universitätsbibliothek Bremen) Antarctic Indian |
institution |
Open Polar |
collection |
Media SuUB Bremen (Staats- und Universitätsbibliothek Bremen) |
op_collection_id |
ftsubbremen |
language |
English |
topic |
Numerical model Sediment transport silt Agulhas Drift Agulhas Plateau Transkei Basin South African Gateway Regional Oceanic Modeling System ROMS Antarctic Bottom Water AABW North Atlantic Deep Water NADW eddy eddy kinetic energy EKE 550 550 Earth sciences and geology ddc:550 |
spellingShingle |
Numerical model Sediment transport silt Agulhas Drift Agulhas Plateau Transkei Basin South African Gateway Regional Oceanic Modeling System ROMS Antarctic Bottom Water AABW North Atlantic Deep Water NADW eddy eddy kinetic energy EKE 550 550 Earth sciences and geology ddc:550 Li, Xin Numerical Simulation of Sediment Transport at the Agulhas Drift on the South African Gateway in relation to its Geodynamic Development |
topic_facet |
Numerical model Sediment transport silt Agulhas Drift Agulhas Plateau Transkei Basin South African Gateway Regional Oceanic Modeling System ROMS Antarctic Bottom Water AABW North Atlantic Deep Water NADW eddy eddy kinetic energy EKE 550 550 Earth sciences and geology ddc:550 |
description |
The South African Gateway is a critical region for the water mass exchange between the Atlantic and the Indian Ocean. The variability in the interoceanic exchange is relevant to global climate change. High resolution seismic reflection data were collected in the Transkei Basin during R/V SONNE cruise SO 182 in 2005. These seismic observations have indicated that a large elongate mounded contourite drift, the Agulhas Drift, has been built up by eastward flows of Antarctic Bottom Water (AABW) and North Atlantic Deep Water (NADW) since about 3 Ma. For a better understanding of the influences of the various currents on sediment transport patterns in the vicinity of the Agulhas Drift, the Regional Oceanic Modeling System (ROMS) has been used to simulate the current system and suspended sediment transport processes. The results from current system simulation showed that a recurrent individual cyclonic eddy event is the key hydrodynamic feature in the Transkei Basin. These eddies are almost fixed in the center of the Transkei Basin and spread over the entire water column. Flow in their northern segments is eastward across the southern flank of the Agulhas Drift. These eddies are supposedly the result of perturbations in the Subtropical Convergence (STC) in the region of south of Africa, where planetary waves on the STC deform. The perturbations enhance the surface eddy kinetic energy (EKE) in the Transkei Basin. The high EKE is then transferred from the surface to the deep ocean, where it causes the formation of eddies at abyssal depth. Based on the ocean circulation simulations, grain size experiments were carried out to test the transport behaviors for 4 different silt grain size classes. Our simulations reveal that sediment transport patterns in the Transkei Basin are strongly influenced by the mesoscale eddies. During eddy events, silts at all tested grain sizes can be resuspended by the AABW along the northeastern flank of the Agulhas Plateau that borders the Transkei Bsin to the east, whereas not all of them can ... |
author2 |
Miller, Heinrich Huhn, Katrin |
format |
Doctoral or Postdoctoral Thesis |
author |
Li, Xin |
author_facet |
Li, Xin |
author_sort |
Li, Xin |
title |
Numerical Simulation of Sediment Transport at the Agulhas Drift on the South African Gateway in relation to its Geodynamic Development |
title_short |
Numerical Simulation of Sediment Transport at the Agulhas Drift on the South African Gateway in relation to its Geodynamic Development |
title_full |
Numerical Simulation of Sediment Transport at the Agulhas Drift on the South African Gateway in relation to its Geodynamic Development |
title_fullStr |
Numerical Simulation of Sediment Transport at the Agulhas Drift on the South African Gateway in relation to its Geodynamic Development |
title_full_unstemmed |
Numerical Simulation of Sediment Transport at the Agulhas Drift on the South African Gateway in relation to its Geodynamic Development |
title_sort |
numerical simulation of sediment transport at the agulhas drift on the south african gateway in relation to its geodynamic development |
publisher |
Universität Bremen |
publishDate |
2012 |
url |
https://media.suub.uni-bremen.de/handle/elib/282 https://nbn-resolving.org/urn:nbn:de:gbv:46-00102528-18 |
geographic |
Antarctic Indian |
geographic_facet |
Antarctic Indian |
genre |
Antarc* Antarctic NADW North Atlantic Deep Water North Atlantic |
genre_facet |
Antarc* Antarctic NADW North Atlantic Deep Water North Atlantic |
op_relation |
https://media.suub.uni-bremen.de/handle/elib/282 urn:nbn:de:gbv:46-00102528-18 |
op_rights |
info:eu-repo/semantics/openAccess |
_version_ |
1766275276467077120 |