|Statement||edited by G. White.|
|Series||WMO/TD -- no. 762., WCRP -- 95., WCRP (Series) -- 95.|
|Contributions||White, Glenn Hazen, 1949-, European Centre for Medium Range Weather Forecasts., World Climate Research Programme.|
|The Physical Object|
|Pagination||xxxiii, 184, 8 p. :|
|Number of Pages||184|
For comparison, the annual mean solar heat flux entering the ocean from the sea surface is above W m —2 on average, corresponding to a net heat input of 50 x 10 8 W. In consequence, it is accurate to consider that the main external forcing of the ocean circulation comes from the free by: Workshop on Air-Sea Flux Fields for Forcing Ocean Model and Validating GCM, WCRP, World Climate Research Program, Geneva, Tang, W., and W.T. Liu, Objective Interpolation of Scatterometer Winds. The resulting datasets, widely referred to as reanalyses, have the benefit that variability in time is not contaminated by the effects of model revisions. Fields from the reanalyses have become widely used both as surface forcing for ocean models and for analyses of atmospheric variability over a broad range of by: AIR-SEA HEAT FLUX, OCEAN WIND FIELDS, AND OFFSHORE DISPERSAL OF GULLS [J Christopher & Lee, David S Haney] on *FREE* shipping on qualifying : Haney, J Christopher & Lee, David S.
WCRP, Proc. WCRP Workshop on Air–Sea Flux Fields for Forcing Ocean Models and Validating GCMs. Geneva, Switzerland, World Climate Research Programme, WCRP, WMO/TD-No. , –Cited by: 3. ICPO Publication Series No. 1, World Climate Research Programme, Geneva, Switzerland, Meehl, G. A., Modification of surface fluxes from component models in global coupled models. Air-Sea Flux Fields for Forcing Ocean Models and Validating GCMs, WCRP, WMO/TD-No. , World Climate Research Programme, Geneva, Switzerland, atmospheric reanalysis products with flux buoy and OceanSITES measurements, including scaling analysis to estimate uncertainties from spatial/temporal variability. • Ocean synthesis and reanalyses should archive components of the air-sea heat flux i.e. Short and Longwave radiation, and sensible and latent heat fluxes, to enable evaluation. 6. Sea And Atmoshere Interaction and Climate Laboratory of P.P. Shirshov Institute Of Oceanology. email: , A. da Silva, , Intercomparison and Validation of Ocean-Atmosphere Flux Fields. Final Report of the WCRP/SCOR Worksing Group on Air-Sea Fluxes. WMO/TD, Geneva, Switserland, pp.
surface forcing has an impact on ocean state estimates even in assimilation mode. This is particularly true prior to the altimetry era – with the paucity of ocean interior observations, much of the time-varying upper ocean state estimate is directly forced by air-sea fluxes. In . MJO-atmospheric river connections and their sensitivity to air-sea coupling across a CESM2 hierarchy: P-A Beraki, Asmerom: Examining the role SH sea-ice forcing on southern Africa rainfall extreme variability: Model sensitivity experiment: P-C Bernardello, Raffaele. WCRP WCRP WORKSHOP ON AIR-SEA FLUX FIELDS FOR FORCING OCEAN MODELS AND VALIDATING GCMS (Reading, UK, October ) (WMO/TD-No. ) (out of print) WCRP NORTHERN HEMISPHERE ATMOSPHERIC BLOCKING AS SIMULATED BY 15 ATMOSPHERIC GENERAL CIRCULATION MODELS IN THE PERIOD (Results from an AMIP Diagnostic . Air Sea fl uxes in operational oceanography and ocean reanalyses. net air-sea heat fluxes used to force ocean models is the. Considering the WCRP-relevant air-sea flux issues in.