Antarctic contribution to meltwater pulse 1A from reduced Southern Ocean overturning.
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Punctuated Shutdown of Atlantic Meridional Overturning Circulation during Greenland Stadial 1Sea-level constraints on the amplitude and source distribution of Meltwater Pulse 1AAbrupt Bølling warming and ice saddle collapse contributions to the Meltwater Pulse 1a rapid sea level rise.Antarctic ice sheet discharge driven by atmosphere-ocean feedbacks at the Last Glacial TerminationClosing the sea level budget at the Last Glacial Maximum.Centennial-scale Holocene climate variations amplified by Antarctic Ice Sheet discharge.Half-metre sea-level fluctuations on centennial timescales from mid-Holocene corals of Southeast AsiaDeglacial temperature history of West Antarctica.Antarctic Cenozoic climate history from sedimentary records: ANDRILL and beyond.West Antarctic Ice Sheet retreat driven by Holocene warm water incursions.Rapid global ocean-atmosphere response to Southern Ocean freshening during the last glacial.Freshening by glacial meltwater enhances melting of ice shelves and reduces formation of Antarctic Bottom Water.Southern Hemisphere westerlies as a driver of the early deglacial atmospheric CO2 rise.Holocene reconfiguration and readvance of the East Antarctic Ice SheetA centuries-long delay between a paleo-ice-shelf collapse and grounding-line retreat in the Whales Deep Basin, eastern Ross Sea, AntarcticaPast continental shelf evolution increased Antarctic ice sheet sensitivity to climatic conditionsThe spatial extent and dynamics of the Antarctic Cold ReversalGlacial isostatic adjustment in response to changing Late Holocene behaviour of ice streams on the Siple Coast, West AntarcticaOcean temperature thresholds for Last Interglacial West Antarctic Ice Sheet collapsePoorly ventilated deep ocean at the Last Glacial Maximum inferred from carbon isotopes: A data-model comparison studyControls on Last Glacial Maximum ice extent in the Weddell Sea embayment, AntarcticaPotential for Southern Hemisphere climate surprisesSensitivity of the Southern Ocean to enhanced regional Antarctic ice sheet meltwater inputDetecting high spatial variability of ice shelf basal mass balance, Roi Baudouin Ice Shelf, AntarcticaEast Antarctic ice sheet most vulnerable to Weddell Sea warmingCollapse of the North American ice saddle 14,500 years ago caused widespread cooling and reduced ocean overturning circulationThe silicon cycle impacted by past ice sheets
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Antarctic contribution to meltwater pulse 1A from reduced Southern Ocean overturning.
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2014 nî lūn-bûn
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2014 թուականի Սեպտեմբերին հրատարակուած գիտական յօդուած
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2014 թվականի սեպտեմբերին հրատարակված գիտական հոդված
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2014年の論文
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2014年論文
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2014年論文
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2014年論文
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2014年論文
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2014年論文
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2014年论文
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Antarctic contribution to meltwater pulse 1A from reduced Southern Ocean overturning.
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Antarctic contribution to meltwater pulse 1A from reduced Southern Ocean overturning.
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Antarctic contribution to meltwater pulse 1A from reduced Southern Ocean overturning.
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label
Antarctic contribution to meltwater pulse 1A from reduced Southern Ocean overturning.
@ast
Antarctic contribution to meltwater pulse 1A from reduced Southern Ocean overturning.
@en
Antarctic contribution to meltwater pulse 1A from reduced Southern Ocean overturning.
@nl
prefLabel
Antarctic contribution to meltwater pulse 1A from reduced Southern Ocean overturning.
@ast
Antarctic contribution to meltwater pulse 1A from reduced Southern Ocean overturning.
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Antarctic contribution to meltwater pulse 1A from reduced Southern Ocean overturning.
@nl
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Antarctic contribution to meltwater pulse 1A from reduced Southern Ocean overturning.
@en
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10.1038/NCOMMS6107
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2014-09-29T00:00:00Z
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1020489863