Research output: Contribution to journal › Article › peer-review
Three-dimensional structure of the mesoscale eddies in the Agulhas Current region from hydrological and altimetry data. / Sandalyuk, N. V.; Belonenko, T. V.
In: Russian Journal of Earth Sciences, Vol. 21, No. 4, ES4005, 07.2021.Research output: Contribution to journal › Article › peer-review
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TY - JOUR
T1 - Three-dimensional structure of the mesoscale eddies in the Agulhas Current region from hydrological and altimetry data
AU - Sandalyuk, N. V.
AU - Belonenko, T. V.
N1 - Publisher Copyright: Copyright 2021 by the Geophysical Center RAS.
PY - 2021/7
Y1 - 2021/7
N2 - In this work by implementing the method of colocalization the altimetry data and temperature and salinity profiles we provide a detailed study of the averaged thermohaline structure of the anticyclonic and cyclonic mesoscale eddies formed in the southern part of the Agulhas Current system. The observed intensification of eddy dissipation processes can be caused by the topographic barriers, such as the Agulhas Plateau or the Agulhas Ridge. In the eddies of both polarities significant temperature anomalies are concentrated within the distance of one radius from the eddy center and to the depth of ∼ 1500 m. The obtained averaged estimates of heat and salt transported by the Agulhas Rings is 2.38×1020 J and 4.79×1012 kg respectively. Westward propagation of the zonal eddy-induced transport for anticyclonic and cyclonic eddies is observed in the Agulhas Retroflection region, Cape Basin and in the central part of the shelf zone with the maximum values of 4 Sv/deg2 for anticyclonic eddies and 1.77 Sv/deg2 for cyclonic eddies.
AB - In this work by implementing the method of colocalization the altimetry data and temperature and salinity profiles we provide a detailed study of the averaged thermohaline structure of the anticyclonic and cyclonic mesoscale eddies formed in the southern part of the Agulhas Current system. The observed intensification of eddy dissipation processes can be caused by the topographic barriers, such as the Agulhas Plateau or the Agulhas Ridge. In the eddies of both polarities significant temperature anomalies are concentrated within the distance of one radius from the eddy center and to the depth of ∼ 1500 m. The obtained averaged estimates of heat and salt transported by the Agulhas Rings is 2.38×1020 J and 4.79×1012 kg respectively. Westward propagation of the zonal eddy-induced transport for anticyclonic and cyclonic eddies is observed in the Agulhas Retroflection region, Cape Basin and in the central part of the shelf zone with the maximum values of 4 Sv/deg2 for anticyclonic eddies and 1.77 Sv/deg2 for cyclonic eddies.
KW - Agulhas current
KW - Agulhas rings
KW - Altimetry
KW - Mesoscale eddies
KW - Three-dimensional structure
KW - SOUTHEAST ATLANTIC-OCEAN
KW - RINGS
KW - SOUTHWEST
KW - mesoscale eddies
KW - TRANSPORT
KW - EVOLUTION
KW - EDDY
KW - three-dimensional structure
KW - Agulhas Rings
KW - Agulhas Current
KW - RETROFLECTION
KW - altimetry
UR - http://www.scopus.com/inward/record.url?scp=85115102735&partnerID=8YFLogxK
UR - https://www.mendeley.com/catalogue/c48a78bf-d696-3388-aadf-6e45463fb99e/
U2 - 10.2205/2021ES000764
DO - 10.2205/2021ES000764
M3 - Article
AN - SCOPUS:85115102735
VL - 21
JO - Russian Journal of Earth Sciences
JF - Russian Journal of Earth Sciences
SN - 1681-1178
IS - 4
M1 - ES4005
ER -
ID: 85331509