Ice in the Southern Ocean is sensitive to various types of climate change. Anthropogenic global warming threatens ice shelves that hang off the Antarctic coastlines, along with the marine communities that inhabit them, via ice sheet thinning and, in extreme cases, ice shelf collapse (Mayewski et al., 2009). Global-warming-induced climate change, working in tandem with the now recovering ozone hole, has contributed to a positive trend in the Southern Annular Mode (SAM) (e.g., Fyfe et al., 2007), which leads to a poleward shift in the mid-latitude westerly winds (Spence et al., 2014). A poleward shift in the westerlies tends to weaken the polar easterly winds, which help to maintain the Antarctic Slope Front, a dynamical oceanic barrier preventing significant heat exchange on the Antarctic continental shelf with relatively warm circumpolar deep water (Spence et al., 2014). The strength and positioning of this front in response to changes in the winds can be highly consequential for Antarctic sea ice, as intrusions of circumpolar deep water onto the continental shelf cause substantial basal melting (Dinniman et al., 2012). Weakened polar easterlies also decrease the amount of downward Ekman