Within a few years, the main outlet glacier draining the region — Zachariae Isstrom — retreated about 20 kilometers, and
regional ice mass loss jumped from zero to roughly 10 metric gigatons a year.
Not exact matches
Rignot et al., Recent Antarctic
ice mass loss from radar interferometry and
regional climate modelling, Nature Geoscience 1, 106 — 110 (2008)
For example, if
ice sheet
mass loss becomes rapid, it is conceivable that the cold fresh water added to the ocean could cause
regional surface cooling [199], perhaps even at a point when sea level rise has only reached a level of the order of a meter [200].
We use realistic estimates of
mass redistribution from
ice mass loss and land water storage to quantify the resulting ocean bottom deformation and its effect on global and
regional ocean volume change estimates.
Mean sea level (MSL) evolution has a direct impact on coastal areas and is a crucial index of climate change since it reflects both the amount of heat added in the ocean and the
mass loss due to land
ice melt (e.g. IPCC, 2013; Dieng et al., 2017) Long - term and inter-annual variations of the sea level are observed at global and
regional scales.