Sentences with phrase «calving front retreats»

«As the glacier's calving front retreats into deeper regions, it loses ice — the ice in front that is holding back the flow — causing it to speed up,» Joughin clarifies.

Not exact matches

RETREATING ICE Jakobshavn Glacier in western Greenland (its front edge, where ice is calving into the ocean, shown here in 2012) is one of the world's fastest - shrinking glaciers.
This means that, even though the glacier is flowing towards the coast and carrying more ice into the ocean, its calving front is actually retreating.
More specifically, using digital scans of paper maps based on aerial imagery acquired by the U.S. Geological Survey, along with modern - day satellite imagery from a variety of platforms, the authors digitized a total of 49 maps and images from which they calculated changes in the terminus positions, ice speed, calving rates and ice front advance and retreat rates from 34 glaciers in this region over the period 1955 - 2015.
Historic photos and maps (from the 1800's to present) indicate a long term retreat of ice calving fronts on Greenland's glaciers.
Is there a point where the mountains ringing Greenland open up such that as the calving fronts continue to retreat, they will begin to greatly widen?
Helheim Glacier is five kilometers wide and at the calving front less than 1 km thick, from 2001 - 2005 it retreated 8 km, you are looking at less than a contribution of 40 km3 for a five kilometer retreat over a span of four years.
According to the NASA map, the retreat of the calving front in the period 1929 - 1953 (24 years) was as large as the retreat in the period 1953 - 2003 (50 years).
Change was afoot: after 50 years of apparent stability, the glacier calving front was retreating, and the grounding line was retreating indicating reduced bedrock anchoring.
This means that, even though the glacier is flowing towards the coast and carrying more ice into the ocean, its calving front is actually retreating, stated the press release.
The acceleration to worry about is from changes in the calving front, and the resultant retreat and acceleration that has been observed on almost all Greenland marine terminating outlet glaciers.
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