The last glacial cycle: transient simulations with an AOGCM
about
The Holocene temperature conundrum.Asynchronous warming and δ18O evolution of deep Atlantic water masses during the last deglaciation.The Transient Response of Ice Volume to Orbital Forcing During the Warm Late PlioceneKinetic energy-conserving hyperdiffusion can improve low resolution atmospheric modelsGlobal warming and ocean stratification: A potential result of large extraterrestrial impacts
P2860
The last glacial cycle: transient simulations with an AOGCM
description
im Januar 2012 veröffentlichter wissenschaftlicher Artikel
@de
wetenschappelijk artikel
@nl
наукова стаття, опублікована в січні 2012
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name
The last glacial cycle: transient simulations with an AOGCM
@en
The last glacial cycle: transient simulations with an AOGCM
@nl
type
label
The last glacial cycle: transient simulations with an AOGCM
@en
The last glacial cycle: transient simulations with an AOGCM
@nl
prefLabel
The last glacial cycle: transient simulations with an AOGCM
@en
The last glacial cycle: transient simulations with an AOGCM
@nl
P2860
P1433
P1476
The last glacial cycle: transient simulations with an AOGCM
@en
P2860
P2888
P304
P356
10.1007/S00382-011-1283-Y
P577
2012-01-12T00:00:00Z