Top-of-atmosphere radiative contribution to unforced decadal global temperature variability in climate models
about
On the definition and identifiability of the alleged "hiatus" in global warming.Earth's energy imbalance since 1960 in observations and CMIP5 models.Spread in the magnitude of climate model interdecadal global temperature variability traced to disagreements over high-latitude oceans.Change in the magnitude and mechanisms of global temperature variability with warming.Regions of significant influence on unforced global mean surface air temperature variability in climate modelsThe necessity of cloud feedback for a basin-scale Atlantic Multidecadal OscillationCombining satellite observations and reanalysis energy transports to estimate global net surface energy fluxes 1985-2012Hiatus-like decades in the absence of equatorial Pacific cooling and accelerated global ocean heat uptakeInvestigating the recent apparent hiatus in surface temperature increases: 1. Construction of two 30-member Earth System Model ensemblesDistinct energy budgets for anthropogenic and natural changes during global warming hiatus
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Top-of-atmosphere radiative contribution to unforced decadal global temperature variability in climate models
description
article
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im Juli 2014 veröffentlichter wissenschaftlicher Artikel
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wetenschappelijk artikel
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наукова стаття, опублікована в липні 2014
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ലേഖനം
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Top-of-atmosphere radiative co ...... variability in climate models
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Top-of-atmosphere radiative co ...... variability in climate models
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Top-of-atmosphere radiative co ...... variability in climate models
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Top-of-atmosphere radiative co ...... variability in climate models
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Top-of-atmosphere radiative co ...... variability in climate models
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Top-of-atmosphere radiative co ...... variability in climate models
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P2093
P2860
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P1476
Top-of-atmosphere radiative co ...... variability in climate models
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P2860
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10.1002/2014GL060625
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2014-07-22T00:00:00Z