Crack in Larsen C ice shelf. Photo: Ted Scambos / NSIDC

By John Abraham
12 June 2017

(The Guardian) – Very soon, a large portion of an ice shelf in Antarctica will break off and collapse into the ocean. The name of the ice shelf is Larsen C; it is a major extension from of the West Antarctic ice sheet, and its health has implications for other ice in the region, and sea levels globally.

How do we know a portion is going to collapse? Well, scientists have been watching a major rift (crack) that has grown in the past few years, carving out a section of floating ice nearly the size of Delaware. The speed of the crack has increased dramatically in the past few months, and it is nearly cracked through. […]

Why does all this matter? Well it is important for a number of reasons. First, when an ice shelf melts or collapses, it can unpin other ice that is sitting on land, which allows it to flow more quickly into the ocean. It is this secondary effect – the loss of ice resting on land – that changes the rate of sea level rise. Loss of a major ice shelf can also activate ice that rests on bedrock topography that makes it fundamentally unstable – ice that, once moving, will move faster and faster, until a large region is afloat.

The entire Larsen Ice shelf, which is the fourth largest in Antarctica, covers nearly 50,000 square km (20,000 square miles) according to reporting at ABC science. The ice on the land upstream of the shelf is enough to raise sea level, eventually, by ten centimeters. This is not, by itself, a major threat to the world’s coastlines, but it reveals the path that other, even larger areas are likely to take in the future. […]

Perhaps a quotation from a seminal work on Antarctic ice sheets best sums up the situation. In a 1978 paper, John Mercer from the Institute of Polar studies concluded:

One of the warning signs that a dangerous warming trend is under way in Antarctica will be the breakup of ice shelves on both coasts of the Antarctic Peninsula, starting with the northernmost and extending gradually southward. These ice shelves should be regularly monitored by LANDSAT imagery.

Why is the ice shelf going to break off and collapse into the ocean? Since large calving events are so rare, and since our measurements in and around ice shelves don’t go back in time far enough, it’s hard to say whether this is a natural progression, variability, or a result of human activity (or more likely a mixture). A major reason may be human-caused warming, which has led to melting from both above and below in nearby areas. The Western Antarctic (the parts south of the U.S.) is warming quite quickly, faster than most of the planet. In addition, warmer waters can reach underneath the ice shelf and can melt it from below. [more]

The Larsen C ice shelf collapse hammers home the reality of climate change

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