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一种新型海-气湍流通量参数化方案的模式测试
引用本文:班军梅,胡艳冰,李煜斌,徐小慧,孙燕.一种新型海-气湍流通量参数化方案的模式测试[J].海洋学报,2010,32(6):72-82.
作者姓名:班军梅  胡艳冰  李煜斌  徐小慧  孙燕
作者单位:1.中国科学院 大气物理研究所 大气边界层物理和大气化学国家重点实验室,北京 100029; 中国科学院研究生院,北京100049
基金项目:国家科技部"973"项目亚印太交汇区海气相互作用(2006CB403600);气候系统模式发展中的关键技术与多模式比较研究(GYHY200806006);中国科学院"百人计划"项目联合资助。
摘    要:将一种新型湍流通量参数化方案代入到大气环流模式CAM3中,对比分析了模式改进前后模拟的风应力、感热通量、潜热通量和降水的全球分布,以及风应力、潜热通量和降水的纬向平均。结果表明:改进后模式的模拟结果更接近ERS、ERA40湍流通量数据和CMAP综合降水数据,其中对西风带上洋面风应力、亚洲季风区的潜热通量和降水改进明显。由于该新型湍流通量参数化方案直接由整体理查逊数、空气动力学粗糙度和热力学粗糙度参数化稳定度参数,避免了通过循环迭代计算Obukhov长度,计算效率得到提高。

关 键 词:CAM3    海-气湍流通量    参数化模拟
收稿时间:2009/4/12 0:00:00
修稿时间:2010/11/19 0:00:00

Model test of a new air-sea turbulent flux parameterization scheme
BAN Jun-mei,HU Yan-bing,LI Yu-bin,XU Xiao-hui and SUN Yan.Model test of a new air-sea turbulent flux parameterization scheme[J].Acta Oceanologica Sinica (in Chinese),2010,32(6):72-82.
Authors:BAN Jun-mei  HU Yan-bing  LI Yu-bin  XU Xiao-hui and SUN Yan
Institution:State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry, Institute of Atmospheric Physics, CAS, Beijing 100029, China; Graduate University of Chinese Academy of Sciences, Beijing 100049, China;State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry, Institute of Atmospheric Physics, CAS, Beijing 100029, China; Institute of Aeronautical Meteorology, Air Force Academy of Equipment, Beijing 100085, China; Shanxi Meteor;State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry, Institute of Atmospheric Physics, CAS, Beijing 100029, China; Graduate University of Chinese Academy of Sciences, Beijing 100049, China;State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry, Institute of Atmospheric Physics, CAS, Beijing 100029, China; Graduate University of Chinese Academy of Sciences, Beijing 100049, China;Shanxi Meteorological Bureau, Taiyuan, 030002, China
Abstract:A new turbulent flux parameterization scheme has been incorporated into the Community Atmosphere Model version3 (CAM3). The global distribution of turbulent fluxes and precipitation, and the zonal means of latent heat flux and precipitation simulated by CAM3 coupled with the new scheme are compared to the counterparts simulated by the original CAM3. The results show that the outputs of the improved model are much more closely to ERS, ERA40 turbulent data and CMAP data than those of the original CAM3 model, especially the wind stress in the Northern Hemisphere trade wind region, and the latent heat flux and precipitation in Asia monsoon. Because the Obukhov stability parameter is parameterized directly by using bulk Richardson number, aerodynamic roughness length, and heat roughness length, the calculate efficiency increased.
Keywords:air-sea surface flux scheme  turbulent fluxes  precipitation
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