globalchange  > 气候变化事实与影响
DOI: 10.1175/JCLI-D-13-00169.1
Scopus记录号: 2-s2.0-84892601126
论文题名:
Origins of the solar radiation biases over the Southern Ocean in CFMIP2 models
作者: Bodas-Salcedo A.; Williams K.D.; Ringer M.A.; Beau I.; Cole J.N.S.; Dufresne J.-L.; Koshiro T.; Stevens B.; Wang Z.; Yokohata T.
刊名: Journal of Climate
ISSN: 8948755
出版年: 2014
卷: 27, 期:1
起始页码: 41
结束页码: 56
语种: 英语
Scopus关键词: Cloud feedbacks ; Cloud properties ; Cloud-aerosol lidar and infrared pathfinder satellite observations ; Extratropical cyclones ; Low-level clouds ; Sea surface temperature (SST) ; Short-wave radiation ; Solar radiation budgets ; Climate models ; Clouds ; Optical radar ; Solar radiation ; Storms ; Sun ; Computer simulation ; CALIPSO ; climate modeling ; cloud ; cyclone ; extratropical environment ; radiation budget ; shortwave radiation ; solar radiation ; Southern Ocean
英文摘要: Current climate models generally reflect too little solar radiation over the Southern Ocean, which may be the leading cause of the prevalent sea surface temperature biases in climate models. The authors study the role of clouds on the radiation biases in atmosphere-only simulations of the Cloud Feedback Model Intercomparison Project phase 2 (CFMIP2), as clouds have a leading role in controlling the solar radiation absorbed at those latitudes. The authors composite daily data around cyclone centers in the latitude band between 40° and 70°S during the summer. They use cloud property estimates from satellite to classify clouds into different regimes, which allow them to relate the cloud regimes and their associated radiative biases to themeteorological conditions in which they occur. The cloud regimes are defined using cloud properties retrieved using passive sensors and may suffer from the errors associated with this type of retrievals. The authors use information from the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) lidar to investigate inmore detail the properties of the "midlevel" cloud regime.Most of the model biases occur in the cold-air side of the cyclone composite, and the cyclone composite accounts formost of the climatological error in that latitudinal band. The midlevel regime is themain contributor to reflected shortwave radiation biases. CALIPSO data show that themidlevel cloud regime is dominated by two main cloud types: cloud with tops actually at midlevel and low-level cloud. Improving the simulation of these cloud types should help reduce the biases in the simulation of the solar radiation budget in the Southern Ocean in climate models. © 2014 American Meteorological Society.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/51073
Appears in Collections:气候变化事实与影响

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作者单位: Met Office Hadley Centre, Exeter, United Kingdom; Météo-France, Toulouse, France; Environment Canada, Toronto, ON, Canada; LMD/IPSL, CNRS, Université Pierre et Marie Curie, Paris, France; Meteorological Research Institute, Japan Meteorological Agency, Tsukuba, Japan; Max Planck Institute for Meteorology, Hamburg, Germany; Beijing Climate Center, China Meteorological Administration, Beijing, China; National Institute for Environmental Studies, Tsukuba, Japan

Recommended Citation:
Bodas-Salcedo A.,Williams K.D.,Ringer M.A.,et al. Origins of the solar radiation biases over the Southern Ocean in CFMIP2 models[J]. Journal of Climate,2014-01-01,27(1)
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