The effect of a dynamic soil scheme on the climate of the mid-Holocene and the Last Glacial Maximum
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Threshold in North Atlantic-Arctic Ocean circulation controlled by the subsidence of the Greenland-Scotland Ridge.Impact of Weddell Sea shelf progradation on Antarctic bottom water formation during the MioceneLate Cretaceous climate simulations with different CO2 levels and subarctic gateway configurations: A model-data comparison
P2860
The effect of a dynamic soil scheme on the climate of the mid-Holocene and the Last Glacial Maximum
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wetenschappelijk artikel
@nl
наукова стаття, опублікована в січні 2016
@uk
name
The effect of a dynamic soil s ...... e and the Last Glacial Maximum
@en
The effect of a dynamic soil s ...... e and the Last Glacial Maximum
@nl
type
label
The effect of a dynamic soil s ...... e and the Last Glacial Maximum
@en
The effect of a dynamic soil s ...... e and the Last Glacial Maximum
@nl
prefLabel
The effect of a dynamic soil s ...... e and the Last Glacial Maximum
@en
The effect of a dynamic soil s ...... e and the Last Glacial Maximum
@nl
P2860
P50
P356
P1433
P1476
The effect of a dynamic soil s ...... e and the Last Glacial Maximum
@en
P2860
P304
P356
10.5194/CP-12-151-2016
P577
2016-01-29T00:00:00Z