skip to main content
OSTI.GOV title logo U.S. Department of Energy
Office of Scientific and Technical Information

Title: Transient response of the Hadley Centre coupled ocean-atmosphere model to increasing carbon dioxide. Part 3: Analysis of global-mean response using simple models

Journal Article · · Journal of Climate
 [1]
  1. Meteorological Office, Bracknell, Berkshire (United Kingdom)

The roles of surface, atmospheric, and oceanic feedbacks in controlling the global-mean transient response of a coupled ocean-atmosphere general circulation model (AOGCM) to increasing carbon dioxide are investigated. The analysis employs a four-box energy balance model (EBM) and an oceanic box-diffusion model (BDM) both tuned to the simulated general circulation model response. The land-sea contrast in the surface warming is explained almost entirely by the shortwave radiative feedbacks associated with changes in cloud and surface albedo. The oceanic thermal inertia delays the response; however, the initial delay is enhanced by increases in Anarctic sea-ice cover, which substantially reduce the effective climate sensitivity of the model in the first half of the 75-year experiment. When driven by the observed anthropogenic greenhouse forcing from the pre-industrial period to present day, the energy balance model overestimates the warming observed over land. However, inclusion of the direct forcing due to anthropogenic tropospheric sulphate aerosol eliminates the land/sea contrast in the response at 1990, leaving the simulated warming over land slightly below the observed value, although the rapid warming observed during the 1980s is well reproduced. The vertical penetration of the oceanic response is small below 1000 m. Within the top 1000 m the effective diffusivities are substantially enhanced by reduced convection and thermohaline overturning, driven by increased precipitation minus evaporation at high latitudes. These changes in ocean heat transport become significant after year 30, whereupon the effective oceanic heat capacity increases substantially, although this increase is partially offset by the effect of changes in the sea-ice margin.

OSTI ID:
57459
Journal Information:
Journal of Climate, Vol. 8, Issue 3; Other Information: PBD: Mar 1995
Country of Publication:
United States
Language:
English

Similar Records

Carbon-nitrogen interactions regulate climate-carbon cycle feedbacks: results from an atmosphere-ocean general circulation model
Journal Article · Thu Jan 01 00:00:00 EST 2009 · Biogeosciences · OSTI ID:57459

Late pleistocene ice age scenarios based on observational evidence
Journal Article · Thu Apr 01 00:00:00 EST 1993 · Journal of Climate; (United States) · OSTI ID:57459

Decadal variability in coupled sea-ice-thermohaline circulation systems
Journal Article · Mon Dec 01 00:00:00 EST 1997 · Journal of Climate · OSTI ID:57459