Velocity increases at Cook Glacier, East Antarctica, linked to ice shelf loss and a subglacial flood event
<p>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...
| المؤلفون الرئيسيون: | , , |
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| التنسيق: | مقال |
| اللغة: | English |
| منشور في: |
Copernicus Publications
2018-10-01
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| سلاسل: | The Cryosphere |
| الوصول للمادة أونلاين: | https://www.the-cryosphere.net/12/3123/2018/tc-12-3123-2018.pdf |