| 西太平洋暖池区海—气通量计算分析 |
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| 引用本文： | 徐天真,陈伯海.西太平洋暖池区海—气通量计算分析[J].中国海洋大学学报(自然科学版),1993(Z2). |
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| 作者姓名： | 徐天真 陈伯海 |
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| 作者单位： | 青岛海洋大学物理海洋研究所 青岛
(徐天真),青岛海洋大学物理海洋研究所 青岛(陈伯海) |
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| 摘 要： | 用J.Launiaimen和T.Vihma提出的近地面层湍流通量计算方法,对我国在1992年11月至1993年2月TOGA—COARE—IOP实验中所获资料计算处理。得出所在站位的海一气间显效、潜热及动量通量。指出西大平洋暖池海区游热通量与显效通量之比为10.14:1;风速大于8m/s后各通量随风速的变化率明显增加;动量与热量的块体通量系数Cd和Ce,h随风速变化有相似的规律;Monin—Obukhov大气稳定度参数Z/L与△T/U_(10)之间有较好的统计关系。
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| 关 键 词： | 海-气通量 块体能量参数 稳定度参数 |
CALCULATION AND ANALYSIS OF AIR-SEA FLUXES IN WARM POOL REGION OF THE WESTERN PACIFIC |
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| Xu Tianzhen Chen Bohai.CALCULATION AND ANALYSIS OF AIR-SEA FLUXES IN WARM POOL REGION OF THE WESTERN PACIFIC[J].Periodical of Ocean University of China,1993(Z2). |
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| Authors: | Xu Tianzhen Chen Bohai |
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| Institution: | Institute of Physical Oceanography |
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| Abstract: | The dara collected by the "Shiyan 3" research vessel in the TOGA-COARE -IOP experiment in 1992-1993 were analysed with the iterative flux - profile method provided by J. Launiainen and T. Vihma. The results show that the ratio of the latent heat flux to the sensible heat flux is 10. 14; the fluxes increase with wind speed more rapidly for wind speed over 8m/s ; the relation of the bulk coefficient Cd with the wind speed is similar to that of Ce and Cb; and there is an obvious statistical relation between |Z/L | and AT/U10. |
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| Keywords: | Air-sea interface flux bulk flux coefficient stability parameter |
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