A GLOBAL CLIMATE MODEL (GENESIS) WITH A LAND-SURFACE TRANSFER SCHEME (LSX) .1. PRESENT CLIMATE SIMULATION

Citation
Sl. Thompson et D. Pollard, A GLOBAL CLIMATE MODEL (GENESIS) WITH A LAND-SURFACE TRANSFER SCHEME (LSX) .1. PRESENT CLIMATE SIMULATION, Journal of climate, 8(4), 1995, pp. 732-761
Citations number
97
Categorie Soggetti
Metereology & Atmospheric Sciences
Journal title
ISSN journal
08948755
Volume
8
Issue
4
Year of publication
1995
Pages
732 - 761
Database
ISI
SICI code
0894-8755(1995)8:4<732:AGCM(W>2.0.ZU;2-7
Abstract
The present-day climatology of a global climate model (GENESIS Version 1.02) is described. The model includes a land-surface transfer compon ent (LSX) that accounts for the physical effects of vegetation. The at mospheric general circulation model is derived from the NCAR CCM1 and modified to include semi-lagrangian transport of water vapor, subgrid plume convection, PBL mixing, a more complex cloud scheme, and a diurn al cycle. The surface models consist of LSX; multilayer models of soil , snow, and sea ice; sea ice dynamics; and a slab mixed layer ocean. B rief descriptions of the current model components are included in an a ppendix. GENESIS is an ongoing project to develop an earth system mode l prototype for global change research. The Version 1.02 climate model has already proved useful in paleoclimate studies. Results of present -day simulations are described using an atmospheric spectral resolutio n of R15 (similar to 4.5 degrees lat X 7.5 degrees long) and a surface -model resolution of 2 degrees X 2 degrees. In general the quality of the simulations is comparable to that of previous coarse-grid models w ith predicted sea-surface temperatures. Most of the errors are attribu ted to coarse atmospheric resolution, inaccurate cloud parameterizatio n, large ocean roughness length, and lack of ocean dynamics. The resul ts are compared with those using a simplified bucket-soil model and cr ude parameterizations of surface albedo and roughness. Although quite similar results are obtained on global scales, significant regional di fferences including surface warming and drying occur in some regions o f Amazonia and northern midlatitude continental interiors.