A high-resolution ocean-atmosphere coupled downscaling of the present climate over California

TitleA high-resolution ocean-atmosphere coupled downscaling of the present climate over California
Publication TypeJournal Article
Year of Publication2014
AuthorsLi H.Q, Kanamitsu M, Hong S.Y, Yoshimura K, Cayan DR, Misra V.
JournalClimate Dynamics
Volume42
Pagination701-714
Date Published2014/02
Type of ArticleArticle
ISBN Number0930-7575
Accession NumberWOS:000330731300009
Keywordscarbon-dioxide; Catalina Eddy; ccsm3; change scenarios; circulation; Coupled model; ocean-atmosphere interaction; part i; Regional climate; regional spectral model; ROMS; RSM; sensitivity; system; united-states; vertical diffusion
Abstract

A fully coupled regional ocean-atmosphere model system that consists of the regional spectral model and the regional ocean modeling system for atmosphere and ocean components, respectively, is applied to downscale the present climate (1985-1994) over California from a global simulation of the Community Climate System Model 3.0 (CCSM3). The horizontal resolution of the regional coupled modeling system is 10 km, while that of the CCSM3 is at a spectral truncation of T85 (approximately 1.4A degrees). The effects of the coupling along the California coast in the boreal summer and winter are highlighted. Evaluation of the sea surface temperature (SST) and 2-m air temperature climatology shows that alleviation of the warm bias along the California coast in the global model output is clear in the regional coupled model run. The 10-m wind is also improved by reducing the northwesterly winds along the coast. The higher resolution coupling effect on the temperature and specific humidity is the largest near the surface, while the significant impact on the wind magnitude appears at a height of approximately 850-hPa heights. The frequency of the Catalina Eddy and its duration are increased by more than 60% in the coupled downscaling, which is attributed to enhanced offshore sea-breeze. Our study indicates that coupling is vital to regional climate downscaling of mesoscale phenomena over coastal areas.

DOI10.1007/s00382-013-1670-7
Short TitleClim. Dyn.
Student Publication: 
No
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