The ice field represents the remnant of
an even bigger ice sheet from the last glacial period, and now feeds dozens of glaciers across the continent.
Not exact matches
Even relatively large calving events, where tabular
ice chunks the size of Manhattan or
bigger calve from the seaward front of the shelf, can be considered normal if the
ice sheet is in overall balance.
The
ice sheets themselves are the
biggest challenge for climate modelling since we don't have direct evidence of the many of the key processes that occur at the
ice sheet base (for obvious reasons), nor
even of what the topography or conditions are at the base itself.