Current models
suggest ice mass losses increase with temperature more rapidly than gains due to increased precipitation and that the surface mass balance becomes negative (net ice loss) at a global average warming (relative to pre-industrial values) in excess of 1.9 to 4.6 °C.
Not exact matches
Joughin et al. (2010) applied a numerical
ice sheet model to predicting the future of PIG, their model
suggested ongoing
loss of
ice mass from PIG, with a maximum rate of global sea level rise of 2.7 cm per century.
al)
suggest radiative
loss to space, but they also include references relating to warming bottom water, deepening tropical gyre warm bowls, and increased
mass loss from the Antarctic and Geenland
ice sheets.
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).
We
suggest that
mass loss from disintegrating
ice sheets probably can be approximated better by exponential
mass loss than by linear
mass loss.
Additionally, unadjusted GRACE gravity data has
suggested no lost
ice mass and all estimates of
ice gains or
loss depend on which Glacial Isostatic Adjustments modelers choose to use.
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.
Estimates of the decadal variability in
ice sheet
mass loss (11)
suggest the impact on acceleration estimates is ∼ 0.014 mm / y2 for a 25 - y time series, in the absence of rapid dynamical changes in the
ice sheets.