In northwestern Greenland, glaciers upsurge from a categorical ice piece to a sea in see-sawing anniversary patterns. The ice generally flows faster in a summer than in a winter, and a ends of glaciers, projecting into a ocean, also allege and shelter with a seasons.
A new research shows some critical connectors between these anniversary patterns, sea ice cover and longer-term trends. Glaciologists wish a findings, supposed for announcement in a Jun book of a American Geophysical Union’s Journal of Geophysical Research-Earth Surface and accessible online, will strew light on how a warming Greenland will minister to sea turn rise.
“Rising sea turn can be tough on coastal communities, with aloft charge surges, larger flooding and saltwater intrusion on uninformed water,” pronounced lead author Twila Moon, a researcher during a National Snow and Ice Data Center (NSIDC), partial of a Cooperative Institute for Research in Environmental Sciences (CIRES) during a University of Colorado Boulder. “We know that sea turn will go adult in a future. The plea is to know how fast it will rise, and one component of that is improved bargain how Greenland glaciers behave.”
Moon and colleagues from a University of Washington focused on 16 glaciers in northwest Greenland, collecting minute information on glacier speed, confine position (the “end” of a glacier in a ocean) and sea ice conditions from 2009 to 2014.
Sea ice had an critical change on a glaciers: When a waters in front of a glacier were totally lonesome by sea ice, a ends of a glaciers mostly modernized divided from a land; and icebergs – that differently competence have damaged off and floated divided – stayed attached. When sea ice pennyless adult in a spring, a ends of a glaciers customarily fast retreated toward land as icebergs pennyless away.
By contrast, anniversary swings in glacier speed had small to do with sea ice conditions or glacier confine location. Rather, a speed (or velocity) of ice upsurge is expected responding to changes in a aspect warp on tip of a ice piece and a transformation of meltwater by and underneath a ice sheet.
Over a longer term, however, Moon and her colleagues found a parsimonious attribute between a speed of glaciers and confine location. When sea ice levels were generally low and glaciers’ toes (or termini) retreated some-more than normal and afterwards didn’t re-advance, a glaciers sped up, relocating ice toward a sea some-more quickly. While low sea ice is expected not a full means of a changes, it might be a manifest denote of other processes, such as subsurface ice melt, that also impact confine retreat, Moon said.
It’s critical to commend that a mechanisms pushing anniversary glacier changes in northwestern Greenland and around a universe are not indispensably a same ones pushing longer-term trends, Moon said. Knowing a differences might assistance researchers improved expect a impact of anomalously low sea ice years, for example.
“We do know we’re going to see sea ice rebate in this area, and it’s probable we can start to guess how that might impact glacier velocities,” Moon said.
It’s also possible, she said, that researchers and communities meddlesome in long-term freezing changes—the kind that impact sea levels—may not need to concentration as most on anniversary allege and shelter of a rivers of ice.
“It might be that we need to compensate some-more courtesy instead to these out-of-bounds events, these supernatural years of really low sea ice or really high warp that expected have a biggest change on longer-term trends.”
Source: University of Colorado Boulder