dc.contributor.author |
Rouault, Marjolaine J
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|
dc.contributor.author |
Mouche, A
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|
dc.contributor.author |
Collard, F
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|
dc.contributor.author |
Johannessen, JA
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|
dc.contributor.author |
Chapron, B
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dc.date.accessioned |
2011-05-11T10:52:24Z |
|
dc.date.available |
2011-05-11T10:52:24Z |
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dc.date.issued |
2010-10 |
|
dc.identifier.citation |
Rouault, M.J., Mouche, A., Collard, F., et al. 2010. Mapping the Agulhas Current from space: an assessment of ASAR surface current velocities. Journal of Geophysical Research, Vol. 115, pp 14 |
en_US |
dc.identifier.issn |
0148-0227 |
|
dc.identifier.uri |
http://www.agu.org/pubs/crossref/2010/2009JC006050.shtml
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dc.identifier.uri |
http://hdl.handle.net/10204/4999
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dc.description |
Copyright: 2010 American Geophysical Union |
en_US |
dc.description.abstract |
Over 2 years of surface current information collected in the Agulhas Current region and derived from the Doppler centroid anomalies of Envisat’s advanced synthetic aperture radar (ASAR) are examined. The sources of errors and potential use of ASAR surface current velocities for oceanographic research are assessed. ASAR surface current velocities are compared to surface drifter data and merged altimetry observations. Maps of sea surface temperature are used to establish the ASAR’s capacity to capture the synoptic circulation. Discrepancies between observed and predicted ASAR velocities result predominantly from inadequate wind corrections combined with radar incidence angles below 30°. Occasionally observed wind-induced outliers cause a bias in the estimated ASAR velocities but do not affect the ability of the ASAR to systematically image regions of strong surface current flow and shear. Time-averaged maps of ASAR-derived surface current velocity seem able to accurately capture the position as well as the intensity of the Agulhas Current. The ability of the ASAR to pick up the smaller features of the circulation along the shelf break also shows that variability along the Agulhas Bank is of the same order of magnitude as that observed in the Agulhas retroflection. ASAR surface current velocities offer a very good complement to altimetry in regions where the mean dynamic topography is poorly resolved. The quasi-synoptic nature of ASAR acquisitions combined with the relatively high resolution of ASAR surface current velocities also make it attractive for studies of submesoscale processes and western boundary current dynamics. |
en_US |
dc.language.iso |
en |
en_US |
dc.publisher |
American Geophysical Union |
en_US |
dc.relation.ispartofseries |
Workflow request;5127 |
|
dc.subject |
Agulhas current |
en_US |
dc.subject |
Agulhas bank |
en_US |
dc.subject |
ASAR |
en_US |
dc.subject |
Agulhas retroflection |
en_US |
dc.subject |
Surface current velocities |
en_US |
dc.subject |
Synoptic maps |
en_US |
dc.subject |
Geophysical |
en_US |
dc.title |
Mapping the Agulhas Current from space: an assessment of ASAR surface current velocities |
en_US |
dc.type |
Article |
en_US |
dc.identifier.apacitation |
Rouault, M. J., Mouche, A., Collard, F., Johannessen, J., & Chapron, B. (2010). Mapping the Agulhas Current from space: an assessment of ASAR surface current velocities. http://hdl.handle.net/10204/4999 |
en_ZA |
dc.identifier.chicagocitation |
Rouault, Marjolaine J, A Mouche, F Collard, JA Johannessen, and B Chapron "Mapping the Agulhas Current from space: an assessment of ASAR surface current velocities." (2010) http://hdl.handle.net/10204/4999 |
en_ZA |
dc.identifier.vancouvercitation |
Rouault MJ, Mouche A, Collard F, Johannessen J, Chapron B. Mapping the Agulhas Current from space: an assessment of ASAR surface current velocities. 2010; http://hdl.handle.net/10204/4999. |
en_ZA |
dc.identifier.ris |
TY - Article
AU - Rouault, Marjolaine J
AU - Mouche, A
AU - Collard, F
AU - Johannessen, JA
AU - Chapron, B
AB - Over 2 years of surface current information collected in the Agulhas Current region and derived from the Doppler centroid anomalies of Envisat’s advanced synthetic aperture radar (ASAR) are examined. The sources of errors and potential use of ASAR surface current velocities for oceanographic research are assessed. ASAR surface current velocities are compared to surface drifter data and merged altimetry observations. Maps of sea surface temperature are used to establish the ASAR’s capacity to capture the synoptic circulation. Discrepancies between observed and predicted ASAR velocities result predominantly from inadequate wind corrections combined with radar incidence angles below 30°. Occasionally observed wind-induced outliers cause a bias in the estimated ASAR velocities but do not affect the ability of the ASAR to systematically image regions of strong surface current flow and shear. Time-averaged maps of ASAR-derived surface current velocity seem able to accurately capture the position as well as the intensity of the Agulhas Current. The ability of the ASAR to pick up the smaller features of the circulation along the shelf break also shows that variability along the Agulhas Bank is of the same order of magnitude as that observed in the Agulhas retroflection. ASAR surface current velocities offer a very good complement to altimetry in regions where the mean dynamic topography is poorly resolved. The quasi-synoptic nature of ASAR acquisitions combined with the relatively high resolution of ASAR surface current velocities also make it attractive for studies of submesoscale processes and western boundary current dynamics.
DA - 2010-10
DB - ResearchSpace
DP - CSIR
KW - Agulhas current
KW - Agulhas bank
KW - ASAR
KW - Agulhas retroflection
KW - Surface current velocities
KW - Synoptic maps
KW - Geophysical
LK - https://researchspace.csir.co.za
PY - 2010
SM - 0148-0227
T1 - Mapping the Agulhas Current from space: an assessment of ASAR surface current velocities
TI - Mapping the Agulhas Current from space: an assessment of ASAR surface current velocities
UR - http://hdl.handle.net/10204/4999
ER -
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en_ZA |