Science Source

Ocean heat drives rapid basal melt of the Totten Ice Shelf

States that mass loss from the West Antarctic ice shelves and glaciers has been linked to basal melt by ocean heat flux
States that the Totten Ice Shelf in East Antarctica, which buttresses a marine-based ice sheet with a volume equivalent to at least 3.5 m of global sea-level rise, also experiences rapid basal melt, but the role of ocean forcing was not known because of a lack of observations near the ice shelf
Observations from the Totten calving front confirm that (0.22 ± 0.07) × 106 m3 s−1 of warm water enters the cavity through a newly discovered deep channel
Finds that the ocean heat transport into the cavity is sufficient to support the large basal melt rates inferred from glaciological observations
Concludes that change in ocean heat flux is a plausible physical mechanism to explain past and projected changes in this sector of the East Antarctic Ice Sheet and its contribution to sea level