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Seasonal variability in the Agulhas Retroflection region

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Field Value
Title Seasonal variability in the Agulhas Retroflection region
Names Matano, Ricardo P. (creator)
Simionato, C. G. (creator)
de Ruijter, W. P. (creator)
van Leeween, P. J. (creator)
Strub, P. Ted (creator)
Chelton, Dudley B. (creator)
Schlax, M. G. (creator)
Date Issued 1998-12-01 (iso8601)
Note copyrighted by American Geophysical Union
Abstract The objective of this article is to present evidence for
the existence of seasonal variability in sea surface height
(SSH) anomaly in the Agulhas Retroflection region.
TOPEX/POSEIDON altimeter data are used to estimate
seasonal changes in the mesoscale SSH variability.
There is a seasonal oscillation of SSH variability characterized
by a maximum during the austral summer and a
minimum during the austral winter. The amplitude of
this seasonal change is approximately 30% of its mean
value. During the winter season the spatial distribution
of SSH variability resembles that of the annual mean
variability, with relative maxima centered at approximately
18°F, 27°F and 38°F. During the summer there
is an additional maximum which extends from approximately
20°F to 25°F and from 40° to 42°S. Analysis
of longitude-time diagrams reveals that at low latitudes
planetary waves propagate freely throughout the
basin. Along the latitude of the Agulhas Retroflection
region, the East Madagascar Ridge hampers the westward
propagation of planetary waves. It is speculated
that the difference between summer and winter patterns
is caused by an inertially driven bifurcation of the Agulhas
Current.
Genre Article
Identifier Chelton, D. B., de Ruijter, W. P., Matano R. P., Schlax, M. G. Simionato, C. G., Strub, P.T., van Leeuween, P. J., 1998, Seasonal variability in the Agulhas Retroflection region: Geophys. Res. Lett, v.23, p4361-4364.

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