8/11/2019 Underlying Ocean Melts Ice Shelf, Speeds Up Glacier Movement

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Underlying ocean melts ice shelf, speeds upglacier movement

Warm ocean water, not warm air, is melting the Pine Island Glacier's floating ice

shelf in Antarctica and may be the culprit(th phm)for increased melting ofother ice shelves, according to an international team of researchers. "We've been

dumping heat into the atmosphere for years and the oceans have been doing

their job, taking it out of the air and into the ocean," said Sridhar Anandakrishnan,

professor of geosciences, Penn State. "Eventually, with all that atmospheric heat,

the oceans will heat up."

The researchers looked at the remote Pine Island Glacier, a major outlet of the

West Antarctic Ice Sheet because it has rapidly thinned and accelerated in therecent past.

"It has taken years and years to do the logistics because it is so remote from

established permanent bases," said Anandakrishnan.

Pine Island Glacier or PIG lies far from McMurdo base, the usual location of

American research in Antarctica. Work done in the southern hemisphere's

summer, December through January 2012-13, included drilling holes in the ice to

place a variety of instruments and using radar to map the underside(mt bndi)of the ice shelf and the bottom of the ocean. Penn State researchers didthe geophysics for the project and the research team's results are reported today

(Sept. 13) in Science.

The ice shelf is melting more rapidly from below for a number of reasons. The

oceans are warmer than they have been in the past and water can transfer more

heat than air. More importantly, the terrain(a hnh)beneath the ice shelf is aseries of channels. The floating ice in the channel has ample room beneath it for

ocean water to flow in. The water melts some of the ice beneath and cools. If the

water remained in the channel, the water would eventually cool to a point whereit was not melting much ice, but the channels allow the water to flow out to the

open ocean and warmer water to flow in, again melting the ice shelf from

beneath.

8/11/2019 Underlying Ocean Melts Ice Shelf, Speeds Up Glacier Movement

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"The way the ocean water is melting the ice shelf is a deeply non-uniform way,"

said Anandakrishnan. "That's going to be more effective in breaking these ice

shelves apart."

The breaking apart of the ice shelf in the channels is similar to removing an icejam from a river. The shelf was plugging(bt ,chn)the channel, but once it isgone, the glacier moves more rapidly toward the sea, forming more ice shelf, but

removing large amounts of ice from the glacier.

The melting of floating ice shelves does not contribute to sea level rise because

once they are in the water, the ice shelves have already contributed to sea level

rise. However, most of the Antarctic glaciers are on land, and rapidly adding new

ice shelf material to the floating mass will increase sea level rise.

"Antarctica is relatively stable, but that won't last forever, said Anandakrishnan.

"This is a harbinger of what will happen."

The researchers believe that the interaction of the ocean beneath the ice shelf

and melting of the ice shelf is an important variable that should be incorporated

into the sea level rise models of global warming. Other recent research shows

that without the channelized underbelly(khu vc d b tn cng)of the ice shelfand glacier, melting would be even more rapid.

"The Antarctic has been relatively quiet as a contributor to sea rise," said

Anandakrishnan. "What this work shows is that we have been blind to a huge

phenomenon, something that will be as big a player in sea level rise in the next

century as any other contributor