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The polar amplification asymmetry: role of Antarctic surface height
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The polar amplification asymmetry: role of Antarctic surface height
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Technical note: Determining Arctic Ocean cold halocline and cold halostad layer...
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Technical note: Determining Arctic Ocean cold halocline and cold halostad layer...
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Technical note: Determining Arctic Ocean halocline and cold halostad depths base...
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Technical note: Determining Arctic Ocean halocline and cold halostad depths base...
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Relative contributions of local heat storage and ocean heat transport to cold‐se...
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Arctic Ocean Surface Energy Flux and the Cold 2 Halocline in Future Climate Proj...
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Arctic Ocean Surface Energy Flux and the Cold Halocline in Future Climate Projec...
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Arctic Ocean Surface Energy Flux and the Cold Halocline in Future Climate Projec...
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CO2-forced changes of Arctic temperature lapse rates in CMIP5 models
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Arctic clouds in ECHAM6 and their sensitivity to cloud microphysics and surface...
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Arctic clouds in ECHAM6 and their sensitivity to cloud microphysics and surface...
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CO2-forced changes of Arctic temperature lapse rates in CMIP5 models
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Climate models disagree on the sign of total radiative feedback in the Arctic
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CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on t...
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CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on t...
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CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on t...
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CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on t...
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CMIP5 simulations of the Max Planck Institute for Meteorology (MPI-M) based on t...
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CMIP5
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IPCC-DDC
climate simulation
decadals
CMIP5_RCM_forcing_MPI-ESM
CORDEX
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ddc:551.46
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Arctic amplification
Atmospheric Science
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