Figure 10. Topex/Poseidon and ERS-2 satellite altimetry analysis for April 20, 1998. Positive and negtive anomalies associated with baroclinicity correspond to regions of a deep and shallow upper layer, respectively. The contour line equidistance is 5 cm.
This figure is reproduced with the kind permission of the Colorado Center for Astrodynamics Research, Dept. of Aerospace Engineering Sciences, University of Colorado, Boulder.
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