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Constraining an Ocean Model Under Getz Ice Shelf, Antarctica, Using A Gravity‐Derived Bathymetry

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Academic year: 2021

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Figure 1. (a) Free ‐ air gravity anomaly over the Getz Ice Shelf, West Antarctica with subregions Getz East (Getz E.), Central (Getz C.), and West (Getz W.) overlaid on a MODIS mosaic of Antarctica
Figure 2. Basal melt rates calculated from the ocean model (average for the years 2006 – 2008) for Case I (a), II (b), and III (c)
Figure 3. Modeled circulation of warm water on the continental shelf for years 2006 – 2008

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