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AOGCM

AOGCM

Chemistry

Atmosphere-ocean General Circulation Model

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AOGCM

General circulation model

surface temperatures as boundary conditions. Coupled atmosphere-ocean GCMs (AOGCMs, e.g. HadCM3, EdGCM, GFDL CM2.X, ARPEGE-Climat) combine the two models.

HadCM3

Model, version 3) is a coupled atmosphere-ocean general circulation model (AOGCM) developed at the Hadley Centre in the United Kingdom. It was one of the

Arctic ice pack

(2002). "Recent and future changes in Arctic sea ice simulated by the HadCM3 AOGCM". Geophysical Research Letters. 29 (24): 28–1–28–4. Bibcode:2002GeoRL..29

Retreat of glaciers since 1850

(October 6, 2010). "The Northeast Asia mountain glaciers in the near future by AOGCM scenarios". The Cryosphere. 4 (4): 435–445. Bibcode:2010TCry....4..435A

Global cooling

the THC weakens, there is still warming over Europe. For example, in all AOGCM integrations where the radiative forcing is increasing, the sign of the

Climate model

surface temperatures as boundary conditions. Coupled atmosphere-ocean GCMs (AOGCMs, e.g. HadCM3, EdGCM, GFDL CM2.X, ARPEGE-Climat) combine the two models.

Timeline of volcanism on Earth

G.S., Gregory, J.M., Scott, P.A., Tett, S.F.B., Thorpe, R.B., 2005. An AOGCM model of the climate response to a volcanic super-eruption. Climate Dynamics

EdGCM

Space Studies NCAR Community Climate System Model NOAA GFDL CM2.X Earth Simulator HadCM3 - explanation of an AOGCM EdGCM at Columbia University v t e

Volcanic impacts on the oceans

Gregory, J. M., Stott, P. a., Tett, S. F. B., & Thorpe, R. B. (2005). An AOGCM simulation of the climate response to a volcanic super-eruption. Climate

Effects of climate change on the water cycle

Models (GCMs) and more recently Atmosphere-Ocean General Circulation Models (AOGCMs) simulate the global circulations and the effects of changes such as an