West Antarctic ice streams

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Effect of Ocean Warming on West Antarctic Ice Streams and Ice Shelves

The Intergovernmental Panel on Climate Change (IPCC) has deemed the Western Antarctic Ice Sheet (WAIS) as very likely to have contributed to sea level rice over the past two decades, estimating a loss of 44 ±13 Gt/yr. Focus has shifted to the behavior and dynamics of the WAIS ice streams since ~90 % of the outward ice flux flows through the ice streams. The behavior and movement of the ice stre...

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West Antarctic Ice Sheet Initiative

The ocean's influence upon and response to Antarctic ice sheet changes is considered in relation to sea level rise over recent and future decades. Assuming present-day ice fronts are in approximate equilibrium, a preliminary budget for the ice sheet is estimated from accumulation vs. iceberg calving and the basal melting that occurs beneath floating ice shelves. Iceberg calving is derived from ...

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Bacteria beneath the West Antarctic ice sheet.

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Comparing ice discharge through West Antarctic Gateways

Introduction Conclusions References Tables Figures

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Shear heating and weakening of the margins of West Antarctic ice streams

Ice streams are fast flowing bands of ice separated from stagnant ridges by shear margins. The mechanisms controlling the location of the margins remain unclear. We use published ice deformation data and a simple one-dimensional thermal model to show that West Antarctic ice stream margins have temperate ice over a substantial fraction of their thickness, a condition that may control their width...

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ژورنال

عنوان ژورنال: Reviews of Geophysics

سال: 1977

ISSN: 8755-1209

DOI: 10.1029/rg015i001p00001