Walker,, Dziga P.; Brandon, Mark A.; Jenkins, Adrian; Allen, John T.; Dowdeswell, Julian A. and Evans, Jeff
(2007).
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| DOI (Digital Object Identifier) Link: | https://doi.org/10.1029/2006GL028154 |
|---|---|
| Google Scholar: | Look up in Google Scholar |
Abstract
Glaciers which drain the West Antarctic Ice Sheet
(WAIS) into the Amundsen Sea are accelerating and
thinning rapidly. These observations have been attributed
to the regional oceanography whereby heat contained within
Circumpolar Deep Water (CDW) drives the basal melting of
floating glaciers. On the basis of new data we calculate that
2.8 terra-Watts (1012) of oceanic heat flow onto the
continental shelf and toward the glaciers via a submarine
glacial trough. This is enough to account for most of the
basal melting in the entire region suggesting the ocean is
supplying an excess of heat toward the Antarctic continent.
| Item Type: | Article |
|---|---|
| ISSN: | 0094-8276 |
| Keywords: | HEAT TRANSPORT;PINE ISLAND BAY; oceanography; Antarctic ice sheet |
| Academic Unit/School: | Faculty of Science, Technology, Engineering and Mathematics (STEM) > Environment, Earth and Ecosystem Sciences Faculty of Science, Technology, Engineering and Mathematics (STEM) |
| Interdisciplinary Research Centre: | Centre for Earth, Planetary, Space and Astronomical Research (CEPSAR) |
| Item ID: | 8714 |
| Depositing User: | Mark Brandon |
| Date Deposited: | 20 Jul 2007 |
| Last Modified: | 30 Jun 2017 05:48 |
| URI: | http://oro.open.ac.uk/id/eprint/8714 |
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