Rapid bottom melting widespread near Antarctic Ice Sheet grounding lines.
about
Climate change and trace gasesIce-shelf collapse from subsurface warming as a trigger for Heinrich eventsA chemotrophic ecosystem found beneath Antarctic Ice ShelfIncreased future ice discharge from Antarctica owing to higher snowfall.How warm was the last interglacial? New model-data comparisons.Climate change. Understanding glacier flow in changing times.Antarctic ice-sheet loss driven by basal melting of ice shelves.Ice-shelf melting around Antarctica.Antarctic contribution to meltwater pulse 1A from reduced Southern Ocean overturning.Rapid submarine ice melting in the grounding zones of ice shelves in West Antarctica.Ice-sheet response to oceanic forcing.Calving fluxes and basal melt rates of Antarctic ice shelves.The environment and evolution of the West Antarctic ice sheet: setting the stage.Changes in ice dynamics and mass balance of the Antarctic ice sheet.Wind causes Totten Ice Shelf melt and acceleration.Fast retreat of Zachariæ Isstrøm, northeast Greenland.Oceanography. How ice shelves melt.Interhemispheric ice-sheet synchronicity during the Last Glacial Maximum.Observations of change in the Southern Ocean.Ice Sheet Model Intercomparison Project (ISMIP6) contribution to CMIP6.Warm ocean is eroding West Antarctic Ice SheetClimate sensitivity in the AnthropoceneMarine Ice Sheet Collapse Potentially Under Way for the Thwaites Glacier Basin, West AntarcticaA centuries-long delay between a paleo-ice-shelf collapse and grounding-line retreat in the Whales Deep Basin, eastern Ross Sea, AntarcticaIce sheet sources of sea level rise and freshwater discharge during the last deglaciationFree-drifting icebergs: hot spots of chemical and biological enrichment in the Weddell SeaBathymetry of the Amundsen Sea continental shelf: Implications for geology, oceanography, and glaciologyLinear response functions to project contributions to future sea levelOceanic processes as potential trigger and amplifying mechanisms for Heinrich eventsStability of the West Antarctic ice sheet in a warming worldModeling the basal melting and marine ice accretion of the Amery Ice ShelfMarine ice sheet model performance depends on basal sliding physics and sub-shelf meltingProvenance changes between recent and glacial-time sediments in the Amundsen Sea embayment, West Antarctica: clay mineral assemblage evidenceOceanic controls on the mass balance of Wilkins Ice Shelf, AntarcticaSimulation of subice shelf melt rates in a general circulation model: Velocity-dependent transfer and the role of frictionCoupling of ice-shelf melting and buttressing is a key process in ice-sheets dynamicsClimate and biogeochemical response to a rapid melting of the West Antarctic Ice Sheet during interglacials and implications for future climateInability of stratospheric sulfate aerosol injections to preserve the West Antarctic Ice SheetCryospheric Contributions to Sea-Level Rise and VariabilityHigh basal melting forming a channel at the grounding line of Ross Ice Shelf, Antarctica
P2860
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P2860
Rapid bottom melting widespread near Antarctic Ice Sheet grounding lines.
description
2002 nî lūn-bûn
@nan
2002年の論文
@ja
2002年学术文章
@wuu
2002年学术文章
@zh
2002年学术文章
@zh-cn
2002年学术文章
@zh-hans
2002年学术文章
@zh-my
2002年学术文章
@zh-sg
2002年學術文章
@yue
2002年學術文章
@zh-hant
name
Rapid bottom melting widespread near Antarctic Ice Sheet grounding lines.
@en
Rapid bottom melting widespread near Antarctic Ice Sheet grounding lines.
@nl
type
label
Rapid bottom melting widespread near Antarctic Ice Sheet grounding lines.
@en
Rapid bottom melting widespread near Antarctic Ice Sheet grounding lines.
@nl
prefLabel
Rapid bottom melting widespread near Antarctic Ice Sheet grounding lines.
@en
Rapid bottom melting widespread near Antarctic Ice Sheet grounding lines.
@nl
P356
P1433
P1476
Rapid bottom melting widespread near Antarctic Ice Sheet grounding lines.
@en
P2093
Stanley S Jacobs
P304
P356
10.1126/SCIENCE.1070942
P407
P50
P577
2002-06-01T00:00:00Z