Publication Date:
2017-12-14
Description:
Surface melt and subsequent firn air depletion can ultimately
lead to disintegration of Antarctic ice shelves1,2 causing
grounded glaciers to accelerate3 and sea level to rise. In
the Antarctic Peninsula, foehn winds enhance melting near
the grounding line4, which in the recent past has led to the
disintegration of the most northerly ice shelves5,6. Here, we
provide observational and model evidence that this process
also occurs over an East Antarctic ice shelf, where meltwaterinduced
firn air depletion is found in the grounding zone.
Unlike the Antarctic Peninsula, where foehn events originate
from episodic interaction of the circumpolar westerlies with
the topography, in coastal East Antarctica high temperatures
are caused by persistent katabatic winds originating from the
ice sheet’s interior. Katabatic winds warm and mix the air
as it flows downward and cause widespread snow erosion,
explaining 〉3 K higher near-surface temperatures in summer
and surface melt doubling in the grounding zone compared with
its surroundings. Additionally, these winds expose blue ice and
firn with lower surface albedo, further enhancing melt. The
in situ observation of supraglacial flow and englacial storage
of meltwater suggests that ice-shelf grounding zones in East
Antarctica, like their Antarctic Peninsula counterparts, are
vulnerable to hydrofracturing7.
Repository Name:
EPIC Alfred Wegener Institut
Type:
Article
,
isiRev
Format:
application/pdf
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