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A STUDY ON LOW-LEVEL ATMOSPHERIC STRUCTURE ON THE SEASIDE BORDERS TO THE WEST OF HAIKOU

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  • In this paper, the observed data of low-level wind and temperature collected from western outskirts of Haikou city, Hainan Island, are analysed. Mean boundary layer structure, generation and development of ground-level inversion and inner boundary layer on the coastal area of interest, which is in China,s northern tropical area, are analysed. It is found that an inner thermal boundary layer can be produced under intense insolation in both dry and rainy seasons, and the mixing layer on the coast is remarkably deeper than that of inland.
  • [1] Li Zongkai,Pan Yunsian, Sun Runqiao et al.,1985. Meteorological principles of air pollution and their applications. Beijing:Meteorological Publishing House, 82-105 (in Chinese).
    [2] Liang Hanming, Dong Baoqun, Peng Xian'an et al.,1992. An analysis on the characteristics of the mixing layer in the area of the Pearl River Delta. Meteorological Monthly, 18:7-11 (in Chinese).
    [3] Wu Zuchang,Dong Baoqun,Ren Zhenhai et al.,1991. Mean Structure of the low level atmosphere over Neilingding islet and the neighbouring sea. Journnl of Tropicnl Meteorology, 7:162-169(in Chinese).
    [4] Xiang Kezong,1986. Meteorological conditions in boundary layer over Guangdong and its influence on air pollution. Journal of Tropical Meteorology, 2:226-232 (in Chinese).

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Wu Dui. A STUDY ON LOW-LEVEL ATMOSPHERIC STRUCTURE ON THE SEASIDE BORDERS TO THE WEST OF HAIKOU [J]. Journal of Tropical Meteorology, 1995, 1(1): 75-86.
Wu Dui. A STUDY ON LOW-LEVEL ATMOSPHERIC STRUCTURE ON THE SEASIDE BORDERS TO THE WEST OF HAIKOU [J]. Journal of Tropical Meteorology, 1995, 1(1): 75-86.
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Manuscript History

Manuscript received: 27 April 1994
Manuscript revised: 23 July 1994
通讯作者: 陈斌, bchen63@163.com
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    沈阳化工大学材料科学与工程学院 沈阳 110142

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A STUDY ON LOW-LEVEL ATMOSPHERIC STRUCTURE ON THE SEASIDE BORDERS TO THE WEST OF HAIKOU

Abstract: In this paper, the observed data of low-level wind and temperature collected from western outskirts of Haikou city, Hainan Island, are analysed. Mean boundary layer structure, generation and development of ground-level inversion and inner boundary layer on the coastal area of interest, which is in China,s northern tropical area, are analysed. It is found that an inner thermal boundary layer can be produced under intense insolation in both dry and rainy seasons, and the mixing layer on the coast is remarkably deeper than that of inland.

Wu Dui. A STUDY ON LOW-LEVEL ATMOSPHERIC STRUCTURE ON THE SEASIDE BORDERS TO THE WEST OF HAIKOU [J]. Journal of Tropical Meteorology, 1995, 1(1): 75-86.
Citation: Wu Dui. A STUDY ON LOW-LEVEL ATMOSPHERIC STRUCTURE ON THE SEASIDE BORDERS TO THE WEST OF HAIKOU [J]. Journal of Tropical Meteorology, 1995, 1(1): 75-86.
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