SLA and ADT gradients evaluated from CCAR (Figure 1) and PISTACH data (Figure 2, Figure 3), respectively, along the track 204 of Jason 2.
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Gradients have been evaluated by considering the difference in elevation between 29.5°N and 27.5°N and then dividing by the distance along the track. Such a region off the Mississippi River Bridsfoot represents the area where the freshwater mound formation occurs.
创建时间:
2015-12-02



