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More Bad News From Antarctica
By Ernest Stewart

"This ice shelf has existed for at least 10,000 years, and soon it will be gone." ~~~ Ala Khazendar, NASA's Jet Propulsion Laboratory

A new NASA study finds the last remaining section of Antarctica's Larsen B Ice Shelf, which partially collapsed in 2002, is quickly weakening and is likely to disintegrate completely before the end of the decade.

A team led by Ala Khazendar of NASA's Jet Propulsion Laboratory in Pasadena, California, found the remnant of the Larsen B Ice Shelf is flowing faster, becoming increasingly fragmented and developing large cracks. Two of its tributary glaciers also are flowing faster and thinning rapidly. Khazendar said:

"These are warning signs that the remnant is disintegrating. Although it's fascinating scientifically to have a front-row seat to watch the ice shelf becoming unstable and breaking up, it's bad news for our planet. This ice shelf has existed for at least 10,000 years, and soon it will be gone."

Ice shelves are the gatekeepers for glaciers flowing from Antarctica toward the ocean. Without them, glacial ice enters the ocean faster and accelerates the pace of global sea level rise. This study, the first to look comprehensively at the health of the Larsen B remnant and the glaciers that flow into it, has been published online in The Journal Earth and Planetary Science Letters.

Khazendar's team used data on ice surface elevations and bedrock depths from instrumented aircraft participating in NASA's Operation IceBridge, a multiyear airborne survey campaign that provides unprecedented documentation annually of Antarctica's glaciers, ice shelves and ice sheets. Data on flow speeds came from spaceborne synthetic aperture radars operating since 1997.

Khazendar noted his estimate of the remnant's remaining life span was based on the likely scenario that a huge, widening rift that has formed near the ice shelf's grounding line will eventually crack all the way across. The free-floating remnant will shatter into hundreds of icebergs that will drift away, and the glaciers will rev up for their unhindered move to the sea.

Located on the coast of the Antarctic Peninsula, the Larsen B remnant is about 625 square miles (1,600 square kilometers) in area and about 1,640 feet (500 meters) thick at its thickest point. Its three major tributary glaciers are fed by their own tributaries farther inland.

"What is really surprising about Larsen B is how quickly the changes are taking place," Khazendar said. "Change has been relentless."

The remnant's main tributary glaciers are named Leppard, Flask and Starbuck, the latter two after characters in the novel Moby Dick. The glaciers' thicknesses and flow speeds changed only slightly in the first couple of years following the 2002 collapse, leading researchers to assume they remained stable. The new study revealed, however, that Leppard and Flask glaciers have thinned by 65-72 feet (20-22 meters) and accelerated considerably in the intervening years. The fastest moving part of Flask Glacier had accelerated 36 percent by 2012 to a flow speed of 2,300 feet (700 meters) a year. This is comparable to a car accelerating from 55 to 75 mph.

Flask's acceleration, while the remnant has been weakening, may be just a preview of what will happen when the remnant breaks up completely. After the 2002 Larsen B collapse, the glaciers behind the collapsed part of the shelf accelerated as much as eightfold. This is comparable to a car accelerating from 55 to 440 mph.

The third and smallest glacier, Starbuck, has changed little. Starbuck's channel is narrow compared with those of the other glaciers, and the small glacier is strongly anchored to the bedrock, which, explains its comparative stability.

"This study of the Antarctic Peninsula glaciers provides insights about how ice shelves farther south, which hold much more land ice, will react to a warming climate," said JPL glaciologist Eric Rignot, a co-author of the paper.

The research team included scientists from JPL; the University of California, Irvine; and the University Centre in Svalbard, Norway. You can read the paper "The evolving instability of the remnant Larsen B Ice Shelf and its tributary glaciers" here.

Of course, you don't have to go to the bottom or the top of the world, right here in Washington state you can see global warming at work. While Mount Rainer is a stratovolcano, which is over due for an eruption, that could destroy parts of Seattle, it poses more of threat by melting flooding from it's glaciers. The last flood occurred last November, which forced Mount Rainier National Park officials to temporarily close park access at the Nisqually entrance and impacted plant and animal habitat in its path.

While receding glaciers is nothing new, with global warming intensifying, it is happening more rapidly than scientists have ever seen before. Changes that normally occur over a matter of centuries are transpiring over decades. The Nisqually Glacier, for example, one of Rainier's 28 named glaciers, has been disappearing since 1983. It's currently at a historic minimum and still shrinking at more than 3 feet every 7 days.

Paul Kennard, a National Park Service geomorphologist said, "If you look at it on a graph, it's like a pingpong ball just fell off the edge of the table."

And with these increasing temperatures, glacial ice melt increase the risk of sudden avalanches, floods, bolders, and liquid mud slurries, which can all occur without warning.

Park Service Director Jon Jarvis said, "Climate change is clearly human caused. It is happening now. We can see the impacts, and we need to step up to the facts and take actions."

We are facing the greatest challenge that mankind has ever faced and we're failing miserably. As long as you let the 1% and their lackeys in Congress ignore this threat we'll soon be going the way of the Dodo Birds!


12-19-1985 ~ 06-01-2015
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(c) 2015 Ernest Stewart a.k.a. Uncle Ernie is an unabashed radical, author, stand-up comic, DJ, actor, political pundit and for 13 years was the managing editor and publisher of Issues & Alibis magazine. Visit me on Facebook. Follow me on Twitter.

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Issues & Alibis Vol 15 # 23 (c) 06/05/2015