Modelling Circumpolar Deep Water intrusions on the Amundsen Sea continental shelf, Antarctica

By M. Thoma, A. Jenkins, D. Holland, S. Jacobs. 2008

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Twentieth-century global-mean sea-level rise: is the whole greater than the sum of the parts? (2013, background): “Possibly this could be a consequence of a long-term process (Jenkins et al. 2010), or it might be due to recent incursion of warmer water onto the Antarctic shelf caused by regional wind stress changes (Thoma et al. 2008; Hellmer et al. 2009).”
Antarctic sub-shelf melt rates via PICO (2017, background): “…Mouginot et al., 2014) is associated with high melt rates that result from inflow of relatively warm circumpolar deep water (CDW) in the iceshelf cavities (D. M. Holland et al., 2008; Jacobs et al., 2011; Pritchard et al., 2012; Schmidtko et al., 2014; Hellmer et al., 2017; Thoma et al., 2008).”
The spatial structure of Antarctic biodiversity (2014, background): “Finally the Amundsen Sea shelf may represent an intermediate state where warm tongues of PETER CONVEY ET AL.220 Ecological Monographs Vol. 84, No. 2 R E V IE W S CDW water penetrate, but vary in volume and duration on a variety of time scales (Thoma et al. 2008).”