首页 | 本学科首页   官方微博 | 高级检索  
     检索      


Cloud-Aerosol-Radiation (CAR) ensemble modeling system: Overall accuracy and efficiency
Authors:Feng ZHANG  Xin-Zhong LIANG  ZENG Qingcun  Yu GU  Shenjian SU
Institution:1. Earth System Science Interdisciplinary Center, University of Maryland, College Park, MD 20740, USA;International Center for Climate and Environment Sciences, Institute of Atmospheric Physics,Chinese Academy of Sciences, Beijing 100029
2. Earth System Science Interdisciplinary Center, University of Maryland, College Park, MD 20740, USA;Department of Atmospheric and Oceanic Science, University of Maryland, College Park, MD 20740, USA
3. International Center for Climate and Environment Sciences, Institute of Atmospheric Physics,Chinese Academy of Sciences, Beijing 100029
4. Department of Atmospheric and Oceanic Sciences, Joint Institute for Regional Earth System Science and Engineering,University of California, Los Angeles, CA 90095-1565, USA
5. Earth System Science Interdisciplinary Center, University of Maryland, College Park, MD 20740, USA
Abstract:The Cloud-Aerosol-Radiation (CAR) ensemble modeling system has recently been built to better understand cloud/aerosol/radiation processes and determine the uncertainties caused by different treatments of cloud/aerosol/radiation in climate models. The CAR system comprises a large scheme collection of cloud, aerosol, and radiation processes available in the literature, including those commonly used by the world's leading GCMs. In this study, detailed analyses of the overall accuracy and efficiency of the CAR system were performed. Despite the different observations used, the overall accuracies of the CAR ensemble means were found to be very good for both shortwave (SW) and longwave (LW) radiation calculations. Taking the percentage errors for July 2004 compared to ISCCP (International Satellite Cloud Climatology Project) data over (60N,60S as an example, even among the 448 CAR members selected here, those errors of the CAR ensemble means were only about -0.67% (-0.6 Wm-2) and -0.82% (-2.0 Wm-2) for SW and LW upward fluxes at the top of atmosphere, and 0.06% (0.1 Wm-2) and -2.12% (-7.8 Wm-2) for SW and LW downward fluxes at the surface, respectively. Furthermore, model SW frequency distributions in July 2004 covered the observational ranges entirely, with ensemble means located in the middle of the ranges. Moreover, it was found that the accuracy of radiative transfer calculations can be significantly enhanced by using certain combinations of cloud schemes for the cloud cover fraction, particle effective size, water path, and optical properties, along with better explicit treatments for unresolved cloud structures.
Keywords:cloud radiative forcing  radiation  CAR  ensemble
本文献已被 CNKI 万方数据 SpringerLink 等数据库收录!
点击此处可从《大气科学进展》浏览原始摘要信息
点击此处可从《大气科学进展》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号