Mapping of Upper Ocean Velocity and Transport in the Cape Farewell Area
The global Thermohaline Circulation (THC), driven by fluxes of heat and freshwater at the ocean surface, is known to be intimately involved with majorvanations tn the Earth' climate. The East Greenland Coastal Current (EGCC)together with the East Greenland Current (EGC), represent the major sur...
Main Author: | |
---|---|
Format: | Text |
Language: | English |
Published: |
National Oceanography Centre
2006
|
Subjects: | |
Online Access: | http://ecite.utas.edu.au/125345 |
id |
ftunivtasecite:oai:ecite.utas.edu.au:125345 |
---|---|
record_format |
openpolar |
spelling |
ftunivtasecite:oai:ecite.utas.edu.au:125345 2023-05-15T15:51:49+02:00 Mapping of Upper Ocean Velocity and Transport in the Cape Farewell Area Meyer, A 2006 application/pdf http://ecite.utas.edu.au/125345 en eng National Oceanography Centre http://ecite.utas.edu.au/125345/1/125345 cover and abstract.pdf http://ecite.utas.edu.au/125345/2/Meyer_Master_Thesis_Mapping of upper ocean velocity and transport Cape Farewell_NOC_2006.pdf Meyer, A, Mapping of Upper Ocean Velocity and Transport in the Cape Farewell Area (2006) [Masters Coursework] http://ecite.utas.edu.au/125345 Earth Sciences Oceanography Physical Oceanography Masters Coursework NonPeerReviewed 2006 ftunivtasecite 2019-12-13T22:23:53Z The global Thermohaline Circulation (THC), driven by fluxes of heat and freshwater at the ocean surface, is known to be intimately involved with majorvanations tn the Earth' climate. The East Greenland Coastal Current (EGCC)together with the East Greenland Current (EGC), represent the major surfacecurrents drawing fresh water southwards in the North Atlantic and therefore playan important role in the THC. By identifying and quantifying Sub-Polar oceanprocesses such as the EGC we can consolidate our knowledge on present-dayclimate variability. To do so, hydro graphic data from cruise D298 was analyzedand volume transport calculated. We found that the EGC (initially 8.3 Sv) andthe EGCC (initially 1.6 Sv), merge around Cape Farewell and that 2.2 Sv ofvolume transport is lost in the process. We suggest that a certain volume of theboundary currents is integrated into recirculation cells and that 2 2 Sv isexported southward. Further work is needed on the fresh water fluxes toinvestigate the exact quantity of fresh water exported from the EGC and EGCCinto the North Atlantic. Text Cape Farewell East Greenland east greenland current Greenland North Atlantic eCite UTAS (University of Tasmania) Greenland |
institution |
Open Polar |
collection |
eCite UTAS (University of Tasmania) |
op_collection_id |
ftunivtasecite |
language |
English |
topic |
Earth Sciences Oceanography Physical Oceanography |
spellingShingle |
Earth Sciences Oceanography Physical Oceanography Meyer, A Mapping of Upper Ocean Velocity and Transport in the Cape Farewell Area |
topic_facet |
Earth Sciences Oceanography Physical Oceanography |
description |
The global Thermohaline Circulation (THC), driven by fluxes of heat and freshwater at the ocean surface, is known to be intimately involved with majorvanations tn the Earth' climate. The East Greenland Coastal Current (EGCC)together with the East Greenland Current (EGC), represent the major surfacecurrents drawing fresh water southwards in the North Atlantic and therefore playan important role in the THC. By identifying and quantifying Sub-Polar oceanprocesses such as the EGC we can consolidate our knowledge on present-dayclimate variability. To do so, hydro graphic data from cruise D298 was analyzedand volume transport calculated. We found that the EGC (initially 8.3 Sv) andthe EGCC (initially 1.6 Sv), merge around Cape Farewell and that 2.2 Sv ofvolume transport is lost in the process. We suggest that a certain volume of theboundary currents is integrated into recirculation cells and that 2 2 Sv isexported southward. Further work is needed on the fresh water fluxes toinvestigate the exact quantity of fresh water exported from the EGC and EGCCinto the North Atlantic. |
format |
Text |
author |
Meyer, A |
author_facet |
Meyer, A |
author_sort |
Meyer, A |
title |
Mapping of Upper Ocean Velocity and Transport in the Cape Farewell Area |
title_short |
Mapping of Upper Ocean Velocity and Transport in the Cape Farewell Area |
title_full |
Mapping of Upper Ocean Velocity and Transport in the Cape Farewell Area |
title_fullStr |
Mapping of Upper Ocean Velocity and Transport in the Cape Farewell Area |
title_full_unstemmed |
Mapping of Upper Ocean Velocity and Transport in the Cape Farewell Area |
title_sort |
mapping of upper ocean velocity and transport in the cape farewell area |
publisher |
National Oceanography Centre |
publishDate |
2006 |
url |
http://ecite.utas.edu.au/125345 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Cape Farewell East Greenland east greenland current Greenland North Atlantic |
genre_facet |
Cape Farewell East Greenland east greenland current Greenland North Atlantic |
op_relation |
http://ecite.utas.edu.au/125345/1/125345 cover and abstract.pdf http://ecite.utas.edu.au/125345/2/Meyer_Master_Thesis_Mapping of upper ocean velocity and transport Cape Farewell_NOC_2006.pdf Meyer, A, Mapping of Upper Ocean Velocity and Transport in the Cape Farewell Area (2006) [Masters Coursework] http://ecite.utas.edu.au/125345 |
_version_ |
1766387200851705856 |