Beautiful Glaciers Greenland


The Helheim Glacier (66.4°N, 38°W) is a flow of ice that orginates from the much larger Greenland ice Sheet, through a narrow rift in the coastal mountain range and down into the sea at a rate of several kilometers (miles) per year.


Despite a drastic retreat between 2004 and 2006, Helheim glacier managed to gain a small amount of mass by the end of the period. The Jakobshavn glacier, however, is shedding ice ever faster.


Meanwhile, at Kangerdlugssuaq, mass loss sped up but has since returned to the 2000 rate. These differences, the researchers say, show that simply extrapolating from recent changes is not a reliable way of predicting future ice loss.


The center of the Greenland Ice Sheet is only 240 km (150 miles) inland, and the researchers worry that the effects of the glacier's retreat will continue to move inland, ultimately decreasing the thickness of the whole ice sheet. Overall, the margins of the Greenland Ice Sheet have been thinning by tens of meters over the last decade.


The likely underlying cause of these changes is higher air and water temperatures in the area of Southern Greenland. However, the study also identifies a relationship between the retreating front of outlet glaciers such as Helheim and an increase in the rate of flow (as the front of the glacier retreats it offers less resistance to the glacier's movement).


Greenland's three largest glaciers lost an enormous amount of ice during the past decade, but each has quite different prospects for long-term stability. Ian Howat at Ohio State University in Columbus and his colleagues combined remote-sensing data with meteorological modelling to estimate the amounts of ice gained or lost from the glaciers each month from 2000 to 2010.



The overall Greenland Ice Sheet contains approximately 10 percent of the world's freshwater and is up to 3.2 km (two miles) thick. If the entire Greenland Ice Sheet were to melt it would raise sea level by 5 to 6 meters (15 to 20 feet). Ian Howat and his coauthors also state that the processes which are accelerating the thinning and retreat of Helheim Glacier are occurring at other outlet glaciers along the coastal margins of Greenland.


The dynamic interactions of temperature, glacier flow rates, and ice thickness complicate the modeling of future changes in the Greenland Ice Sheet. These processes are likely to continue to accelerate under prevailing climate change scenarios. After years of melting back at a relatively stable speed, Helheim Glacier in southern Greenland has dramatically accelerated its retreat.


According to a research paper published in the scientific journal Geophysical Research Letters by Ian Howat, I. Joughin, S. Tulaczyk, and S. Gogineni, the glacier's rate of flow has increased from 8 kilometer (km) per year (5 miles per year) in 2000 to 11 km per year (6.8 miles per year) in 2005.


In addition to flowing more rapidly the glacier thinned by 40 meters (130 feet) between 2001 and 2003. The calving front of the glacier − the area where the ice breaks away and falls into the ocean − has retreated by approximately 5 km (3.1 miles).



In the sea, the glacier's weight keeps it firmly resting on the ocean floor, as long as the water depth is less than about nine-tenths of the glacier's thickness. Where the water is deep enough to cause the end of the glacier to float, its front becomes brittle, breaking into numerous icebergs.

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