Velocity increases at Cook Glacier, East Antarctica, linked to ice shelf loss and a subglacial flood event
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Published:2018-10-02
Issue:10
Volume:12
Page:3123-3136
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ISSN:1994-0424
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Container-title:The Cryosphere
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language:en
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Short-container-title:The Cryosphere
Author:
Miles Bertie W. J.ORCID, Stokes Chris R.ORCID, Jamieson Stewart S. R.
Abstract
Abstract. Cook Glacier drains a large proportion of the Wilkes Subglacial Basin in East
Antarctica, a region thought to be vulnerable to marine ice sheet instability
and with potential to make a significant contribution to sea level. Despite
its importance, there have been very few observations of its longer-term
behaviour (e.g. of velocity or changes at its ice front). Here we use a
variety of satellite imagery to produce a time series of ice front position
change from 1947 to 2017 and ice velocity from 1973 to 2017. Cook Glacier has two
distinct outlets (termed East and West), and we observe the near-complete loss
of the Cook West Ice Shelf at some time between 1973 and 1989. This was
associated with a doubling of the velocity of Cook West Glacier, which may
also be linked to previously published reports of inland thinning. The loss
of the Cook West Ice Shelf is surprising given that the present-day
ocean climate conditions in the region are not typically associated with
catastrophic ice shelf loss. However, we speculate that a more intense
ocean climate forcing in the mid-20th century may have been important in
forcing its collapse. Since the loss of the Cook West Ice Shelf, the presence
of landfast sea ice and mélange in the newly formed embayment appears to
be important in stabilizing the glacier front and enabling periodic advances.
We also show that the last calving event at the larger Cook East Ice Shelf
resulted in the retreat of its ice front into a dynamically important portion
of the ice shelf and observe a short-lived increase in velocity of Cook East
between 2006 and 2007, which we link to the drainage of subglacial Lake Cook.
Taken together, these observations suggest that the velocity, and hence
discharge, of Cook Glacier is highly sensitive to changes at its terminus, but
a more detailed process-based analysis of this potentially vulnerable region
requires further oceanic and bathymetric data.
Funder
Natural Environment Research Council
Publisher
Copernicus GmbH
Subject
Earth-Surface Processes,Water Science and Technology
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