Warm ocean driving Antarctic ice loss

The researchers used a satellite laser to measure the thinning occurring on ice shelves - the floating tongues of ice that jut out from the land.
The team’s analysis found the shelves’ shrinkage could not be attributed simply to warmer air temperatures.
Rather, it is warm water getting under the floating ice to melt it from below.
This is leading to a weakening of the shelves, permitting more and more ice to drain from the continent’s interior through tributary glaciers.
Previous studies have already indicated that warmer waters are being driven towards the continent by stronger westerly winds in the Southern Ocean.
The researchers say the new understanding has major implications for their ability to reliably project future sea-level rises as a result of Antarctic ice loss.