Many studies have focused on
mapping ice loss from specific glaciers.
Not exact matches
Aerial
mapping of Kilimanjaro's summit in February 2000 revealed a 33 %
loss of
ice since the last
map in 1989 and an 82 % decline since 1912, says geologist Lonnie Thompson of Ohio State University's Byrd Polar Research Center in Columbus.
Glaciologists worldwide use these and other
maps in modeling the rate of
ice loss in Greenland and projecting future
losses.
Through some very clever technical improvements, McMillan and his colleagues have produced the best
maps of Antarctic
ice -
loss we have ever had.
Just thinking out loud (and I only know enough to be dangerous;), but with IR radiation
mapping during winter, one might be able to infer a sub-surface temperature profile and compare that with mass
loss and
ice sheet thickness.
The
maps suggests growth of parts of coastal East Antarctica, little change in the interior and
ice mass
loss in West Antarctica (basins 18 - 27 and 1) focused on the Amundsen Sea Coast region (basins 20 - 23).
A
map of the glacier is then prepared contoured for the observed gain or
loss of snow or
ice in water equivalent units.
Maps pinpointing regions with the greatest basal melt, 48 highlighted here by red dots, coincide with the greatest
loss of glacier
ice along the Amundsen Sea hot spot.
Buoys provide key observations for
mapping and attributing summer
ice loss: drift, bottom vs. top melt, amount of snow accumulation, nature of ponds (even if anecdotal from web cams), and thickness of level
ice.