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The dependence of the eastward-wind-induced vertical drift in the northern hemisphere is opposite to that in the southern hemisphere. For an intuitive sketch see Figure 5 at http://onlinelibrary.wiley.com/doi/10.1029/2010JA016252/full https://agupubs.onlinelibrary.wiley.com/cms/asset/71c335ca-c05c-4d9d-9d67-b1fbcc74bb31/jgra21124-fig-0005.png

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This page is a summary of: A study of the Weddell Sea Anomaly observed by FORMOSAT-3/COSMIC, Journal of Geophysical Research Atmospheres, December 2009, American Geophysical Union (AGU),
DOI: 10.1029/2009ja014175.
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