The future of ice sheets and sea ice: between reversible retreat and unstoppable loss.
about
Arctic climate tipping pointsThe East Siberian Arctic Shelf: towards further assessment of permafrost-related methane fluxes and role of sea iceCanadian Arctic sea ice reconstructed from bromine in the Greenland NEEM ice coreCatalogue of abrupt shifts in Intergovernmental Panel on Climate Change climate modelsThe State of Climate Negotiations: a personal scientific commentaryTipping elements in the Earth SystemArctic marine mammal population status, sea ice habitat loss, and conservation recommendations for the 21st centuryEbullition and storm-induced methane release from the East Siberian Arctic ShelfDynamics of the last glacial maximum Antarctic ice-sheet and its response to ocean forcing.Trapping Phenomenon Attenuates the Consequences of Tipping Points for Limit Cycles.Greenhouse gas mitigation can reduce sea-ice loss and increase polar bear persistence.Cirrus cloud seeding: a climate engineering mechanism with reduced side effects?Biodiversity of Arctic fishes: first karyological information onGaidropsarus argentatus(Reinhardt, 1837), a new piece to the puzzleLaurentide ice-sheet instability during the last deglaciationRecovery mechanisms of Arctic summer sea icePotential climatic transitions with profound impact on EuropeSeptember Arctic sea ice predicted to disappear near 2°C global warming above presentA review of recent developments in climate change science. Part I: Understanding of future change in the large-scale climate systemMitigation implications of an ice-free summer in the Arctic OceanAnalyzing abrupt and nonlinear climate changes and their impactsThe effects of aggressive mitigation on steric sea level rise and sea ice changesExploring uncertainties in the relationship between temperature, ice volume, and sea level over the past 50 million yearsFalse alarms: How early warning signals falsely predict abrupt sea ice lossTipping elements and climate-economic shocks: Pathways toward integrated assessmentArctic sea-ice evolution as modeled by Max Planck Institute for Meteorology's Earth system modelPredictability of large interannual Arctic sea-ice anomaliesFactors controlling the bifurcation structure of sea ice retreatThe reversibility of sea ice loss in a state-of-the-art climate modelInability of stratospheric sulfate aerosol injections to preserve the West Antarctic Ice SheetProjected decline in spring snow depth on Arctic sea ice caused by progressively later autumn open ocean freeze-up this centuryIce thickness in the Northwest PassageAssessing the forecast skill of Arctic sea ice extent in the GloSea4 seasonal prediction systemA case study of a modelled episode of low Arctic sea iceImproving Multiyear Sea Ice Concentration Estimates with Sea Ice DriftTime variability in the annual cycle of sea ice thickness in the Transpolar DriftThinning of Arctic sea ice observed in Fram Strait: 1990-2011Effects of Arctic Sea Ice Decline on Weather and Climate: A Review
P2860
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P2860
The future of ice sheets and sea ice: between reversible retreat and unstoppable loss.
description
2009 nî lūn-bûn
@nan
2009年の論文
@ja
2009年学术文章
@wuu
2009年学术文章
@zh-cn
2009年学术文章
@zh-hans
2009年学术文章
@zh-my
2009年学术文章
@zh-sg
2009年學術文章
@yue
2009年學術文章
@zh
2009年學術文章
@zh-hant
name
The future of ice sheets and sea ice: between reversible retreat and unstoppable loss.
@en
The future of ice sheets and sea ice: between reversible retreat and unstoppable loss.
@nl
type
label
The future of ice sheets and sea ice: between reversible retreat and unstoppable loss.
@en
The future of ice sheets and sea ice: between reversible retreat and unstoppable loss.
@nl
prefLabel
The future of ice sheets and sea ice: between reversible retreat and unstoppable loss.
@en
The future of ice sheets and sea ice: between reversible retreat and unstoppable loss.
@nl
P2860
P356
P1476
The future of ice sheets and sea ice: between reversible retreat and unstoppable loss.
@en
P2860
P304
20590-20595
P356
10.1073/PNAS.0902356106
P407
P50
P577
2009-11-02T00:00:00Z