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热带西太平洋边界层大气的多逆温层特征
引用本文:李若钝,孙瑞本,武建平.热带西太平洋边界层大气的多逆温层特征[J].热带气象学报,1991,0(4):355-365.
作者姓名:李若钝  孙瑞本  武建平
作者单位:国家海洋局第一海洋研究所
摘    要:本文主要利用第四航次“中美热带西太平洋海气相互作用联合调查”所获得的海洋水文气象及低空大气温度探测资料,分析了热带西太平洋暖水区边界层大气层结特征,指出春季热带西太平洋边界层大气具有多逆温层的层结特征。逆温层个数大多为4个左右,厚度多在30m以上,最厚336m。这一研究结果是关于热带大洋边界层结构观测研究的重要补充。 

收稿时间:1990/12/24 0:00:00
修稿时间:1991/4/10 0:00:00

THE CHARACTERISTICS OF MULTIPLE TEMPERATURE INVERSION LAYERS IN THE ATMOSPHERE OF THE BOUNDARY LAYER OVER TROPICAL WEST PACIFIC
Li Ruodun,Sun Ruiben and Wu Jianping.THE CHARACTERISTICS OF MULTIPLE TEMPERATURE INVERSION LAYERS IN THE ATMOSPHERE OF THE BOUNDARY LAYER OVER TROPICAL WEST PACIFIC[J].Journal of Tropical Meteorology,1991,0(4):355-365.
Authors:Li Ruodun  Sun Ruiben and Wu Jianping
Institution:No. 1 Institute of Oceanography, SOA Qingdao
Abstract:In this paper, atmospheric stratification in the boundary layer for warm pools of the tropical West Pacific are analyzed using the hydrographical, meteorological and low-level atmospheric observations from the 4th cruise of PRC-USA Joint Air-sea Interactions Studies in this part of the o-cean. It is pointed out that the stratification is characterized by multiple temperature inversion layers in spring and there are 4 such layers in most cases, with the usual thickness over 30 m, the largest reaching 336 m. The findings are important addition to the work on the structure of the boundary layer over tropical oceans.
Keywords:
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