Ocean water is coursing under the Antarctic ice sheets.
The ice sheets in water do not raise the ocean level much, because the ice sheet is already under water. The Calving point is where the ice sheet comes form land support, and as the ice sheet moves into the ocean, it plops into the ocean and breaks off from the support of the land. Previous to this report, it was only a theory that ocean water circulated significantly in the Calving are. Salt water can melt ice at lower temperatures than freezing, with salinity. The water temperatures in the calving area, are warm enough to melt ice. As oceans warm, the melting speed will increase. The oceans currents flowing into the calving are indicates that oceans may be providing lubrication for ice movement into the sea, from the land, which raises ocean levels, faster..
"Velocity measurements collected by a lowered acoustic Doppler current profiler (LADCP) confirm that the warm water at the bottom of stations 35 and 36 flows strongly (>0.2 m s−1) into the sub–ice shelf cavity (Fig. 3B). The velocity profile is highly sheared, with weak flow in the cold water above the thermocline near 600 m depth and maximum inflow near the seafloor, where the warmest water is found. The deep flow in the eastern trough (station 41) also flows into the cavity but is substantially weaker
"Therefore, several lines of evidence support the conclusion that rapid basal melt of the TIS (19, 24, 25) is driven by the flux of warm mCDW into the cavity: the presence of warm water at the ice front, the existence of a deep trough providing access of this warm water to the cavity, direct measurements of mass and heat transport into the cavity, the signature of glacial meltwater in the outflow, and exchange rates inferred from the heat budget and satellite-derived basal melt rates. Observations of recent change in some East Antarctic glaciers and ice shelves (16–19) and studies of past (12–14, 28, 29) and future (20, 21) sea levels support the hypothesis of a dynamic EAIS. Our observations confirm the existence of a pathway allowing for communication of ocean anomalies to the TIS cavity, highlighting variation in ocean-driven basal melt as a plausible mechanism to explain past and projected changes in the TIS and the ice sheet it buttresses."
Ocean heat drives rapid basal melt of the Totten Ice Shelf | Science Advances
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