This adds a new concern to
rapid ice sheet retreat.
Not exact matches
This feedback could potentially result in the
rapid loss of parts of the
ice sheet, as grounding lines
retreat along troughs and basins that deepen towards the
ice sheet's interior.
The
rapid shrinkage of glaciers around the Antarctic Peninsula, coupled with the potential for
ice - shelf collapse and grounding line retreat, raises concerns for the future of the West Antarctic Ice Sheet, and this is an area of urgent current research [
ice - shelf collapse and grounding line
retreat, raises concerns for the future of the West Antarctic
Ice Sheet, and this is an area of urgent current research [
Ice Sheet, and this is an area of urgent current research [3].
Recent work has suggested that
rapid retreat is already underway for sections of the West Antarctic
ice sheet, raising the possibility of increasing contributions to sea - level rise.
A study using Earth Remote Sensing satellite radar interferometry (EERS - 1 and -2) observations from 1992 through 2011 finds «a continuous and
rapid retreat of the grounding lines of Pine Island, Thwaites, Haynes, Smith, and Kohler» Glaciers, and the authors conclude that «this sector of West Antarctica is undergoing a marine
ice sheet instability that will significantly contribute to sea level rise in decades to centuries to come» (Rignot et al. 2014).
Geothermal conditions impart a significant control on the
ice sheet's transient response, particularly during phases of
rapid retreat.
Insights from this study suggests that large sectors of contemporary
ice sheets overlying geothermally active regions, such as Siple Coast, Antarctica, and NE Greenland, have the potential to experience
rapid phases of mass loss and deglaciation once initial
retreat is initiated.
The evidence for
rapid climate change is compelling: Sea level rise, Global temperature rise, Warming oceans, Shrinking
ice sheets, Declining Arctic sea
ice, Glacial
retreat, Extreme events, Ocean acidification, Decreased snow cover http://climate.nasa.gov/evidence/ It's changing «rapidly».
Thus, West Antarctica is not the only potential source of
rapid change; part of the East Antarctic
ice sheet is also susceptible to
rapid retreat because of its direct contact with the ocean and because the bed beneath the
ice slopes landward (Fig. 1), which makes it less stable.
Donald D. Blankenship, a senior researcher at UT's Institute for Geophysics (UTIG) and one of the authors of the study, explained that understanding the evolution of the
ice sheet over the East Antarctic landscape as well as its points of vulnerabilities for
rapid retreat allows them to predict what could potentially happen to the region in the coming years.