Pan-ice-sheet glacier terminus change in East Antarctica reveals sensitivity of Wilkes Land to sea-ice changes.
about
Wind causes Totten Ice Shelf melt and acceleration.Southern Ocean warming and Wilkes Land ice sheet retreat during the mid-Miocene.Recent high-resolution Antarctic ice velocity maps reveal increased mass loss in Wilkes Land, East Antarctica.Holocene reconfiguration and readvance of the East Antarctic Ice SheetSimultaneous disintegration of outlet glaciers in Porpoise Bay (Wilkes Land), East Antarctica, driven by sea ice break-upA Review of Recent Changes in Major Marine-Terminating Outlet Glaciers in Northern GreenlandThe Spatial Structure of the 128 ka Antarctic Sea Ice Minimum
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Pan-ice-sheet glacier terminus change in East Antarctica reveals sensitivity of Wilkes Land to sea-ice changes.
description
2016 nî lūn-bûn
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2016年の論文
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2016年論文
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2016年論文
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2016年論文
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2016年論文
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2016年論文
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2016年论文
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2016年论文
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name
Pan-ice-sheet glacier terminus ...... ilkes Land to sea-ice changes.
@en
type
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Pan-ice-sheet glacier terminus ...... ilkes Land to sea-ice changes.
@en
prefLabel
Pan-ice-sheet glacier terminus ...... ilkes Land to sea-ice changes.
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P2860
P356
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Pan-ice-sheet glacier terminus ...... Wilkes Land to sea-ice changes
@en
P2093
Bertie W J Miles
P2860
P304
P356
10.1126/SCIADV.1501350
P577
2016-05-06T00:00:00Z