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Lu Naiping,Li Shiming,Chen Jingnan,Zheng Yueming,Zhou Mingyu. 1989. A calculation method of the sensible heat flux by sodar. Acta Oceanologica Sinica, (2):191-198
A calculation method of the sensible heat flux by sodar
A calculation method of the sensible heat flux by sodar
Received:February 15, 1988  Revised:April 15, 1988
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Author NameAffiliation
Lu Naiping National Recsearch Center for Marine Environmcntul Forecasts, Beijing, China 
Li Shiming National Recsearch Center for Marine Environmcntul Forecasts, Beijing, China 
Chen Jingnan National Recsearch Center for Marine Environmcntul Forecasts, Beijing, China 
Zheng Yueming National Recsearch Center for Marine Environmcntul Forecasts, Beijing, China 
Zhou Mingyu National Recsearch Center for Marine Environmcntul Forecasts, Beijing, China 
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Abstract:
      During the second course of USA-PRC joint air sea interaction experiment in 1986, the temperature structure parameters CT2 were measured by sodar over the Western Pacific Ocean. Based on similarity theory, a method is discussed to calculate the sensible heat flux over the ocean in unstable stratification. Becausehumidity is great over the ocean, so we have to consider the influence of water vapor structure parameter Ce2 and the correlation coefficient betweene and T on the calculation of sensible heat flux using CT2 profiles measured by sodar. A new formula is suggested in terms of parameterization. The sensible heat flux calculated by sodar measurements is compared with that by bulk transfer method, and the results agree well.
中文摘要:
      During the second course of USA-PRC joint air sea interaction experiment in 1986, the temperature structure parameters CT2 were measured by sodar over the Western Pacific Ocean. Based on similarity theory, a method is discussed to calculate the sensible heat flux over the ocean in unstable stratification. Becausehumidity is great over the ocean, so we have to consider the influence of water vapor structure parameter Ce2 and the correlation coefficient betweene and T on the calculation of sensible heat flux using CT2 profiles measured by sodar. A new formula is suggested in terms of parameterization. The sensible heat flux calculated by sodar measurements is compared with that by bulk transfer method, and the results agree well.
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