The PIG is not dominated by its ice shelf, hence the potential for
rapid ice stream response.
Recent glacial history and
rapid ice stream retreat in the Amundsen Sea.
Not exact matches
The data, collected by aerial survey missions flown in the Southern Hemisphere in the summer of 2014 - 2015, provide detailed topography of the perpetually
ice - free region, where surprising landscape changes, such as
rapid erosion along some
streams, have been observed in recent years.
The mechanism for their
rapid movement is being intensively studied because of the possibility that
rapid ice -
stream flow may cause the
ice sheet to disintegrate, resulting in a disastrous rise in world - wide sea level.
The discovery is significant in relation to the mechanism for
rapid movement of the
ice streams, which are huge, fast - flowing
ice currents within the slow - moving
ice sheet that covers most of Antarctica.
The loss of Arctic summer sea
ice and the
rapid warming of the continent could be altering the jet
stream [3]-- and thus weather patterns — over North America, Europe and Russia, increasing the likelihood of extreme weather events and driving winter storms south.
A number of climate scientists are currently investigating the possible link between abnormal jet
streams and the
rapid loss of Arctic sea
ice, which if true would mean climate change may not only be exacerbating heatwaves but cold spells as well.
Recent satellite and in situ observations of
ice streams behind disintegrating
ice shelves highlight some
rapid reactions of
ice sheet systems.