A dynamic early East Antarctic Ice Sheet suggested by ice-covered fjord landscapes.
about
Subglacial Lake Vostok (Antarctica) accretion ice contains a diverse set of sequences from aquatic, marine and sediment-inhabiting bacteria and eukaryaOcean access to a cavity beneath Totten Glacier in East AntarcticaOcean heat drives rapid basal melt of the Totten Ice Shelf.Ecology of subglacial lake vostok (antarctica), based on metagenomic/metatranscriptomic analyses of accretion ice.Pan-ice-sheet glacier terminus change in East Antarctica reveals sensitivity of Wilkes Land to sea-ice changes.Repeated large-scale retreat and advance of Totten Glacier indicated by inland bed erosion.Wind causes Totten Ice Shelf melt and acceleration.Observed thinning of Totten Glacier is linked to coastal polynya variability.Initiation and long-term instability of the East Antarctic Ice Sheet.Geophysics: earth's longest fossil rift-valley system.Climate change: Ancient Antarctic fjords.The distribution of basal water between Antarctic subglacial lakes from radar sounding.Recent high-resolution Antarctic ice velocity maps reveal increased mass loss in Wilkes Land, East Antarctica.Seismic detection of an active subglacial magmatic complex in Marie Byrd Land, AntarcticaSea surface temperature control on the distribution of far-traveled Southern Ocean ice-rafted detritus during the PlioceneIce flow dynamics and mass loss of Totten Glacier, East Antarctica, from 1989 to 2015Simultaneous disintegration of outlet glaciers in Porpoise Bay (Wilkes Land), East Antarctica, driven by sea ice break-upA high-resolution synthetic bed elevation grid of the Antarctic continentThe subglacial geology of Wilkes Land, East AntarcticaEvidence of a hydrological connection between the ice divide and ice sheet margin in the Aurora Subglacial Basin, East AntarcticaAntarctic bedrock topography uncertainty and ice sheet stabilityComparison of measurements from different radio-echo sounding systems and synchronization with the ice core at Dome C, AntarcticaSteep reverse bed slope at the grounding line of the Weddell Sea sector in West AntarcticaGrounding line retreat of Totten Glacier, East Antarctica, 1996 to 2013The surficial and subglacial geomorphology of western Dronning Maud Land, AntarcticaThe glacial geomorphology of the Antarctic ice sheet bed
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P2860
A dynamic early East Antarctic Ice Sheet suggested by ice-covered fjord landscapes.
description
2011 nî lūn-bûn
@nan
2011 թուականի Յունիսին հրատարակուած գիտական յօդուած
@hyw
2011 թվականի հունիսին հրատարակված գիտական հոդված
@hy
2011年の論文
@ja
2011年論文
@yue
2011年論文
@zh-hant
2011年論文
@zh-hk
2011年論文
@zh-mo
2011年論文
@zh-tw
2011年论文
@wuu
name
A dynamic early East Antarctic Ice Sheet suggested by ice-covered fjord landscapes.
@ast
A dynamic early East Antarctic Ice Sheet suggested by ice-covered fjord landscapes.
@en
type
label
A dynamic early East Antarctic Ice Sheet suggested by ice-covered fjord landscapes.
@ast
A dynamic early East Antarctic Ice Sheet suggested by ice-covered fjord landscapes.
@en
prefLabel
A dynamic early East Antarctic Ice Sheet suggested by ice-covered fjord landscapes.
@ast
A dynamic early East Antarctic Ice Sheet suggested by ice-covered fjord landscapes.
@en
P2093
P2860
P50
P356
P1433
P1476
A dynamic early East Antarctic Ice Sheet suggested by ice-covered fjord landscapes.
@en
P2093
Andrew P Wright
David E Sugden
Jamin S Greenbaum
John W Holt
Neal W Young
P2860
P2888
P356
10.1038/NATURE10114
P407
P50
P577
2011-06-01T00:00:00Z
P5875
P6179
1043927833