Message Board

Respected readers, authors and reviewers, you can add comments to this page on any questions about the contribution, review, editing and publication of this journal. We will give you an answer as soon as possible. Thank you for your support!

Full name
E-mail
Phone number
Title
Message
Verification Code
YAN Jun-yue, YAO Hua-dong, LI Jiang-long, TANG Zhi-yi, SHA Wen-yu, JIANG Guo-rong, LI Xun-qiang, XIAO Yi-guo. The air-sea heat exchange at Xisha areas during the onset of southwest monsoon in 2000[J]. Haiyang Xuebao, 2003, 25(4): 18-28.
Citation: YAN Jun-yue, YAO Hua-dong, LI Jiang-long, TANG Zhi-yi, SHA Wen-yu, JIANG Guo-rong, LI Xun-qiang, XIAO Yi-guo. The air-sea heat exchange at Xisha areas during the onset of southwest monsoon in 2000[J]. Haiyang Xuebao, 2003, 25(4): 18-28.

The air-sea heat exchange at Xisha areas during the onset of southwest monsoon in 2000

  • Received Date: 2001-08-24
  • Rev Recd Date: 2002-12-20
  • Using the observational data of the Second SCS Air-Sea Flux Experiment on the Xisha air-sea flux research tower during May 7 to June 17,2000,the radiation budget,latent and sensible heat fluxes and net oceanic heat budgets before and after summer monsoon onset were calculated.It is found that there are considerable changes on air-sea fluxes,especially on latent heat fluxes and net oceanic heat budget after summer monsoon onset.Furthermore,the analyzed results of five synoptic stages are compared and the special characteristics of flux transfer during the different stages around onset of SCS monsoon are discussed.The fluxes change shows that there is an oceanic heat accumulating process in pre-onset and break period and an oceanic heat loss process in the onset period.Also the latent fluxes and water vapor transported to continent can be influenced by the duration and intension of the southwester especially,further influence on the rainfall appearance in China continent.Finally,through comparison of the Xisha fluxes with those obtained from Indian Ocean and western Pacific Ocean,their differences may be seen.It can explain why after monsoon onset,the SST can keep stable values over the SCS while over the Arabian Sea and the Bay of Bengal they decrease quickly.
  • loading
  • 马耀民,王介民,张庆荣,等.南沙海域大气湍流通量输送特征分析[J].高原气象,1997,16(1):45-51.
    许建林,曲绍厚.1997年冬季南海南部海区不同天气过程下的湍流通量输送[J].热带海洋,2000,19(2):19-26.
    闫俊岳,姚华栋,李江龙,等.1998年南海季风爆发期间近海面层大气湍流结构和通量输送的观测研究[J].气候与环境,2000,5(4):447-458.
    闫俊岳.南海西南季风爆发的气候特征[J].气象学报,1997,55(2):176-188.
    贾新兴,吴清吉.热带西太平洋海-气通量和一维海洋混合层之模拟[J].大气科学(台湾),1999,26(2):157-178.
    MOHANTY U C,MOHAN K N.Variability of the Indian summer monsoon in relation to oceanic heat budget over the Indian seas[J].Atmospheric Environment,1990,24(4):823-828.
    ZHANG Xiu-zhi,WEI Min.The study on the relations between moisture flux in East Asian and the South China Sea summer monsoon[J].Acta Meteoroloica Sinica,2003,17(Supp.):46-57.
  • 加载中

Catalog

    通讯作者: 陈斌, bchen63@163.com
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

    1. 本站搜索
    2. 百度学术搜索
    3. 万方数据库搜索
    4. CNKI搜索
    Article views (1022) PDF downloads(948) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return