«Even though we don't see immediate evidence of
ice shelf breakup on the Ross Ice Shelf, everything we've seen up to this point has occurred faster than we expected.
The full effects of
ice shelf breakup on glacier demise will not be known for some time.
Not exact matches
Warm mountain winds are causing extensive winter melting
on the surface of the Larsen C
ice shelf, which could contribute to its
breakup
While researchers quickly linked the
breakup to lakes of meltwater that had accumulated
on the so - called Larsen B
ice shelf's upper surface and then wedged apart deep crevasses, they hadn't come up with a convincing explanation for what triggered the collapse.
«My fieldwork with the support of the InBev - Baillet Latour Fellowship will shed light
on which processes are responsible for this
ice shelf breakup, thereby improving the estimates how, when and where East Antarctica is most vulnerable to global warming.»
«My fieldwork with the support of the InBev - Baillet Latour Fellowship will shed light
on which processes are responsible for this
ice shelf breakup, thereby improving the estimates how, when and where East Antarctica is most vulnerable to global warming» said Lenaerts.
This flow of
ice, fed by the continuous formation of new
ice on land and culminating in the
breakup of the
shelves on the outer fringe and the calving of icebergs, is not new.
Beyond the present danger, scientists warn that — unless the issue of climate change is addressed — we could see the
breakup of larger
ice shelves, which could have a destabilizing effect
on the entire region and possibly the world.
The strong warming of the Antarctic Peninsula has led to the
breakup of large
ice shelves whose presence tended to impede the oceanward flow of mountain glaciers
on the peninsula.
IMO, the strongest argument for sea
ice decline over the last decade for being unusual and at least in part attributable to global warming is this (from Polyakov et al.): The severity of present
ice loss can be highlighted by the
breakup of
ice shelves at the northern coast of Ellesmere Island, which have been stable until recently for at least several thousand years based
on geological data.