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Why is the AMOC Monostable in Coupled General Circulation Models?
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The importance of Canadian Arctic Archipelago gateways for glacial expansion in...
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Sensitivity to Glacial Forcing in the CCSM4
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Biomes simulated by BIOME4 using CESM2 lig127k, midHolocene, and piControl clima...
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Amplified North Atlantic warming in the late Pliocene by changes in Arctic gatew...
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Amplified Late Pliocene terrestrial warmth in northern high latitudes from great...
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Asynchronous warming and δ18O evolution of deep Atlantic water masses during the...
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Abrupt Heinrich Stadial 1 cooling missing in Greenland oxygen isotopes.
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Asynchronous warming and δ18O evolution of deep Atlantic water masses during the...
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Abrupt Heinrich Stadial 1 cooling missing in Greenland oxygen isotopes
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Asynchronous warming and δ 18 O evolution of deep Atlantic water masses during t...
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Abrupt Heinrich Stadial 1 cooling missing in Greenland oxygen isotopes
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Abrupt Heinrich Stadial 1 cooling missing in Greenland oxygen isotopes
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Deglacial variability of South China hydroclimate heavily contributed by autumn...
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The Southern Westerlies during the last glacial maximum in PMIP2 simulations
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The Southern Westerlies during the last glacial maximum in PMIP2 simulations
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How warm was the last interglacial? New model–data comparisons
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Investigating the direct meltwater effect in terrestrial oxygen-isotope paleocli...
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Investigating the direct meltwater effect in terrestrial oxygen-isotope paleocli...
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Investigating the Direct Meltwater Effect in Terrestrial Oxygen-Isotope Paleocli...
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[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology
54 ENVIRONMENTAL SCIENCES
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ATMOSPHERE MODELS
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Atlantic water masses
CHRONOLOGY AICC2012
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