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

2006~2007年北部湾海-气热通量变化特征
引用本文:盛立芳,郑元鑫,陈静静,王丹.2006~2007年北部湾海-气热通量变化特征[J].中国海洋大学学报(自然科学版),2009,39(4).
作者姓名:盛立芳  郑元鑫  陈静静  王丹
作者单位:1. 中国海洋大学海洋-大气相互作用与气候实验室,山东,青岛,266100;中国海洋大学物理海洋教育部重点实验室,山东,青岛,266100
2. 中国海洋大学海洋气象学系,山东,青岛,266100
3. 湖南省气象台,湖南,长沙,410007
摘    要:用2006年夏~2007年秋在北部湾获得的船测气象资料,由块体公式计算了海-气通量.结果表明:北部湾春、夏季节获得热通量,而秋、冬季节失去热通量.春季通过湍流交换造成的热通量对海面热平衡的贡献最小,其次是夏季、冬季和秋季.在年平均尺度上感热通量和潜热通量分别占净辐射通量的7.4%和77.4%,15.2%的净辐射热量通过海洋过程消耗掉.感热通量随海-气温差的加大而增大,而与风速之间呈现复杂的非线性关系.海-气温差增加1 ℃,感热通量增加6.7~12.7 W/m2;较大的感热通量(>30 W/m2)容易出现在5~10 m/s风速条件下.潜热通量与风速和相对湿度呈明显的相关关系:风速增加1 m/s,潜热通量增加约18 W/m2,而相对湿度下降1%会导致6 W/m2潜热通量的增加.

关 键 词:热通量  北部湾  辐射

Characteristics of Air-Sea Heat Flux in Beibu Gulf in 2006~2007
SHENG Li-Fang,ZHENG Yuan-Xin,CHEN Jing-Jing,WANG Dan.Characteristics of Air-Sea Heat Flux in Beibu Gulf in 2006~2007[J].Periodical of Ocean University of China,2009,39(4).
Authors:SHENG Li-Fang  ZHENG Yuan-Xin  CHEN Jing-Jing  WANG Dan
Institution:Ocean University of China 1.Ocean-Atmosphere Interaction and Climate Laboratary;2.Physical Oceanography Laboratary;3.Marine Meteorology Department;Qingdao 266100;China;4.Meteorological Observatory of Hunan;Changsha 410007;China
Abstract:Air-sea flux in Beibu Gulf was calculated by bulk formulae with vessel-measured meteorological data from Summer 2006 to Autumn 2007.The calculation showed that Beibu Gulf gained net heat flux in spring and summer,lost net heat flux in autumn and winter.The contribution of heat flux caused by turbulence exchange to the heat balance of sea surface was minimum in Spring,and maximum in Autumn. On the annual average scale,sensible heat flux was 7.4% of the net radiation flux,and latent heat flux was 77.4%.15.6% ...
Keywords:COARE3  0  heat flux  Beibu Gulf  COARE3  0  radiation
本文献已被 CNKI 万方数据 等数据库收录!
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