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我国大陆地区和近海海域能量收支分布及其季节变化的数值模拟研究
引用本文:周明煜,李诗明,钱粉兰,陈陟,苏立荣,袁耀初,潘晓玲.我国大陆地区和近海海域能量收支分布及其季节变化的数值模拟研究[J].地球物理学报,2002,45(3):319-329.
作者姓名:周明煜  李诗明  钱粉兰  陈陟  苏立荣  袁耀初  潘晓玲
作者单位:1. 国家海洋环境预报中心,北京,100081; 2. 第二海洋研究所,杭州,310012; 3. 新疆大学,乌鲁木齐,830046
基金项目:国家重点基金项目 (4 973 62 0 0 ),国家自然科学基金项目 (4 0 0 75 0 0 1 ),国家 973项目 (G1 9990 43 5 0 3 )、,国家攀登B项目 (TIPEX)资助
摘    要:应用美国宇航局Goddard地球观测系统四维资料同化系统、计算了我国大陆地区和近海海域1998年各月月平均能量收支各项和10m气温、比湿及风矢量的地理分布特征. 模式计算结果表明,地表短波净辐射最强出现在夏季(7月)新疆和西藏中部地区,高值中心区可达275W/m2,在黄海东海海域春季(4月)最大,其值为250W/m2左右. 地表长波净辐射最强出现在夏季(7月)我国西北地区,中心区值为125W/m2,我国近海海域在冬季(1月)最强,其值为75-100W/m2. 我国近海海面,冬季(1月)潜热通量值高于一般月份,中心区值可达250W/m2,夏季我国大陆西南、华北和东北一带为潜热通量高值区,其值为125W/m2. 月平均能量收支计算结果显示,在黄海、东海海域冬季(1月)净通量为海洋向大气输送,夏季(7月)则反之,新疆和西藏高原中部夏季为净通量正值区. 综合温度、湿度和风矢量场分布发现,夏季从南海向华东地区,孟加拉湾向印度次大陆有明显的水汽平流输送,西藏西南部也有来自西南方向的水汽输送.

关 键 词:能量收支  数值模拟  中国大陆地区  近中国海域.  
文章编号:0001-5733(2002)03-0319-11
收稿时间:2001-07-05

NUMERICAL SIMULATION OF ENERGY BUDGET DISTRIBU-TION AND ITS SEASONAL VARIATION IN CHINA MAINLAND AND SEA AREAS
ZHOU MING YU \ LI SHI MING QIAN FEN LAN \ CHEN ZHI \ SU LI RONG YUAN YAO CHU \ PAN XIAO LING National Center for Marine Environmental Forecasts,Beijing ,China Second Institute of.NUMERICAL SIMULATION OF ENERGY BUDGET DISTRIBU-TION AND ITS SEASONAL VARIATION IN CHINA MAINLAND AND SEA AREAS[J].Chinese Journal of Geophysics,2002,45(3):319-329.
Authors:ZHOU MING YU \ LI SHI MING QIAN FEN LAN \ CHEN ZHI \ SU LI RONG YUAN YAO CHU \ PAN XIAO LING National Center for Marine Environmental Forecasts  Beijing  China Second Institute of
Institution:1. National Center for Marine Environmental Forecasts, Beijing 100081, China; 2. Second Institute of Oceanography, Hangzhou 310012, China; 3. Xinjiang University, Urumqi 830046, China
Abstract:The monthly mean values of energy budget, air temperature, specific humidity and wind vector at 10m over China mainland and sea areas for 1998 were calculated based on Goddard Earth Observing Data Assimilation System, NASA, United States. The results show that the largest net radiation of surface short wave appears in summer (July) in central areas of Xinjiang and Xizang, the magnitude in the high value central area reaches 275W/m 2. The largest net radiation appears in spring (April) in Yellow Sea and East China Sea, its maximum value is about 250W/m 2. The largest net radiation of the surface long wave appears in summer (July) in northwestern China, the value of the central area is 125W/m 2, and it appears in winter (January) in near China sea areas, the value is 75-100W/m 2. The latent heat flux in near China sea areas in winter (January) is higher than that in other months, its value in the central area occurs in southwestern, northern and northeastern China, its value is 125W/m 2. The calculation results of monthly mean energy budget illustrate that the net flux is transferred from ocean to atmosphere in winter (January) in Yellow Sea and East China Sea, and conversely in summer (July). The net flux value is positive in summer in Xinjiang and the central area of Xizang Plateau. The comprehensive analysis for distributions of temperature, humidity and wind vector shows that the water vapour is transported distinctly in summer from South China Sea to eastern China area and from Bay of Bengal to India subcontinent. The water vapour in southwestern area of Xizang comes from its southwestern direction.
Keywords:Energy budget  Numercial simulation  China land area  Near China sea areas  
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