and therefore to be able to make a stronger statement on how unique the current and apparently global warming
related ice mass loss is» for Greenland, he says.
Not exact matches
«Once you have that combination of ocean heat and atmospheric heat — which are
related — that's when the
ice sheet could really experience dramatic
ice mass loss.»
The reconstructed curve includes isolated rapid events of several decimetres within a few centuries, one of which is most likely
related to
loss from the Antarctic
ice sheet
mass around 5000 years before present.
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.