Yangxin Chen

Jun 4, 2024 | agupubs.onlinelibrary.wiley.com | John Moore |Chao Yue |Yangxin Chen |Svetlana Jevrejeva

1 Introduction Ice shelves tend to breakup and retreat when they are exposed to increased basal melt rates via ingress of relative warm, dense deep water derived from Circumpolar Deep Water (CDW) to their grounding lines (Liu et al., 2015; Turner et al., 2017). These deep warm currents circulate around Antarctica offshore of the continental shelf break.