| Lu Naiping,Li Shiming,Chen Jingnan,Zheng Yueming,Zhou Mingyu.A calculation method of the sensible heat flux by sodar[J].Acta Oceanologica Sinica,1989,(2):191-198 |
| A calculation method of the sensible heat flux by sodar |
| A calculation method of the sensible heat flux by sodar |
| 投稿时间：1988-02-15 修订日期：1988-04-15 |
| DOI： |
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| 英文关键词: |
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| 作者 | 单位 | | 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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| 摘要点击次数: 719 |
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| 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. |
| 英文摘要: |
| 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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