Ocean circulation and climate during the past 120,000 years.
about
Coupled biophysical global ocean model and molecular genetic analyses identify multiple introductions of cryptogenic speciesBuried iceberg scours reveal reduced North Atlantic Current during the stage 12 deglacialOverlooked possibility of a collapsed Atlantic Meridional Overturning Circulation in warming climateIsotopic disequilibrium in Globigerina bulloides and carbon isotope response to productivity increase in Southern OceanTemporal Dynamics of Avian Populations during Pleistocene Revealed by Whole-Genome SequencesA Southern Ocean trigger for Northwest Pacific ventilation during the Holocene?Response of Atlantic overturning to future warming in a coupled atmosphere-ocean-ice sheet modelShifts in the spring herring (Clupea harengus membras) larvae and related environment in the eastern Baltic Sea over the past 50 years.Changing currents: a strategy for understanding and predicting the changing ocean circulation.Abrupt glacial climate shifts controlled by ice sheet changes.Earth science: Ocean circulation and rapid climate change.Increased productivity in the subantarctic ocean during Heinrich events.Was millennial scale climate change during the Last Glacial triggered by explosive volcanism?North Atlantic ocean circulation and abrupt climate change during the last glaciation.Tipping elements in the Earth's climate system.Human-induced Arctic moistening.Biodiversity trends along the western European marginOCEAN CIRCULATION. Observing the Atlantic Meridional Overturning Circulation yields a decade of inevitable surprises.Recent colonization of the Galápagos by the tree Geoffroea spinosa Jacq. (Leguminosae).'Back to the future': how archaeological remains can describe salmon adaptation to climate change.Critical slowing down as early warning for the onset of collapse in mutualistic communities.Breathing, crawling, budding, and splitting of a liquid droplet under laser heating.Annually resolved North Atlantic marine climate over the last millennium.On the stability of the Atlantic meridional overturning circulationTrapping Phenomenon Attenuates the Consequences of Tipping Points for Limit Cycles.Climate strategies: thinking through Arctic examples.Palaeoclimatic insights into forcing and response of monsoon rainfall.Endospores of thermophilic bacteria as tracers of microbial dispersal by ocean currents.Subglacial floods beneath ice sheets.231Pa/230Th evidence for a weakened but persistent Atlantic meridional overturning circulation during Heinrich Stadial 1.PALEOCEANOGRAPHY. A warm and poorly ventilated deep Arctic Mediterranean during the last glacial period.Asynchronous demographic responses to Pleistocene climate change in Eastern Nearctic vertebrates.Climate mediates the success of migration strategies in a marine predator.Shrubs tracing sea surface temperature--Calluna vulgaris on the Faroe Islands.Coupled European and Greenland last glacial dust activity driven by North Atlantic climate.Predicting tipping points in mutualistic networks through dimension reduction.Stochastic models of the meridional overturning circulation: time scales and patterns of variability.One-to-one coupling of glacial climate variability in Greenland and Antarctica.Climate change: tropical flip-flop connections.Strong hemispheric coupling of glacial climate through freshwater discharge and ocean circulation.
P2860
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P2860
Ocean circulation and climate during the past 120,000 years.
description
2002 nî lūn-bûn
@nan
2002 թուականի Սեպտեմբերին հրատարակուած գիտական յօդուած
@hyw
2002 թվականի սեպտեմբերին հրատարակված գիտական հոդված
@hy
2002年の論文
@ja
2002年論文
@yue
2002年論文
@zh-hant
2002年論文
@zh-hk
2002年論文
@zh-mo
2002年論文
@zh-tw
2002年论文
@wuu
name
Ocean circulation and climate during the past 120,000 years.
@ast
Ocean circulation and climate during the past 120,000 years.
@en
Ocean circulation and climate during the past 120,000 years.
@nl
type
label
Ocean circulation and climate during the past 120,000 years.
@ast
Ocean circulation and climate during the past 120,000 years.
@en
Ocean circulation and climate during the past 120,000 years.
@nl
prefLabel
Ocean circulation and climate during the past 120,000 years.
@ast
Ocean circulation and climate during the past 120,000 years.
@en
Ocean circulation and climate during the past 120,000 years.
@nl
P2860
P356
P1433
P1476
Ocean circulation and climate during the past 120,000 years.
@en
P2860
P2888
P304
P356
10.1038/NATURE01090
P407
P577
2002-09-01T00:00:00Z