The climate of 6000 years BP in near-equilibrium simulations with a coupled AOGCM

Geophysical Research Letters

Volumn 28, Issue 11, 2001, Pages 2213-2216

  Voss, R ^a   Mikolajewicz, U ^a  

^a MAX PLANCK INSTITUTE FOR METEOROLOGY   (Germany)

Author keywords

[No Author keywords available]

Indexed keywords

BOUNDARY CONDITIONS; CARBON DIOXIDE; COMPUTER SIMULATION; EARTH ATMOSPHERE; ATMOSPHERIC THERMODYNAMICS; OCEANOGRAPHY; UPPER ATMOSPHERE;

MONSOON;

CLIMATE CHANGE;

ATMOSPHERE-OCEAN COUPLING; CLIMATE CHANGE; GENERAL CIRCULATION MODEL; GLOBAL CHANGE; HOLOCENE;

ATMOSPHERE GENERAL CIRCULATION MODELS; COUPLED ATMOSPHERE OCEAN GENERAL CIRCULATION MODEL; EQUILIBRIUM SIMULATIONS; INDIAN MONSOON; OCEAN CIRCULATION; QUASI EQUILIBRIUM; TOTAL RESPONSE; UPPER OCEAN;

EID: 0035365205     PISSN: 00948276     EISSN: None     Source Type: Journal    
DOI: 10.1029/2000GL012498     Document Type: Article

References (11)

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4. A fully coupled GCM simulation of the climate of the mid-Holocene
5. Biome reconstruction from pollen and plant macrofossil data for Africa and the Arabian peninsula at 0 and 6000 years
6. Status of the Paleoclimate Modeling Intercomparison Project (PMIP)
7. Monsoon changes for 6000 years ago: Results of 18 simulations from the Paleoclimate Modeling Intercomparison Project (PMIP)
8. Response of the African monsoon to orbital forcing and ocean feedback in the middle Holocene
9. Multiple-century response of a coupled ocean-atmosphere model to an increase of the atmospheric carbon dioxide
10. Periodically synchronously coupled integrations with the atmosphere-ocean general circulation model ECHAM3/LSG
11. 2 concentration in the coupled atmosphere-ocean general circulation model ECHAM3/LSG