«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.