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首页> 外文期刊>Advances in Meteorology >Upper Ocean Thermal Responses to Sea Spray Mediated Turbulent Fluxes during Typhoon Passage
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Upper Ocean Thermal Responses to Sea Spray Mediated Turbulent Fluxes during Typhoon Passage

机译:台风过境期间上层海洋对海浪介导的湍流通量的热响应

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摘要

A one-dimensional turbulent model is used to investigate the effect of sea spray mediated turbulent fluxes on upper ocean temperature during the passage of typhoon Yagi over the Kuroshio Extension area in 2006. Both a macroscopical sea spray momentum flux algorithm and a microphysical heat and moisture flux algorithm are included in this turbulent model. Numerical results show that the model can well reproduce the upper ocean temperature, which is consistent with the data from the Kuroshio Extension Observatory. Besides, the sea surface temperature is decreased by about 0.5 degrees C during the typhoon passage, which also agrees with the sea surface temperature dataset derived from Advanced Microwave Scanning Radiometer for the Earth Observing and Reynolds. Diagnostic analysis indicates that sea spray acts as an additional source of the air-sea turbulent fluxes and plays a key role in increasing the turbulent kinetic energy in the upper ocean, which enhances the temperature diffusion there. Therefore, sea spray is also an important factor in determining the upper mixed layer depth during the typhoon passage.
机译:利用一维湍流模型研究了2006年黑潮延伸地区台风八木经过时海浪介导的湍流对上层海洋温度的影响。宏观海浪动量通量算法和微观物理热湿通量算法包含在该湍流模型中。数值结果表明,该模型可以很好地再现上层海洋温度,与黑潮扩展天文台的数据一致。此外,台风通过期间海面温度下降了约0.5摄氏度,这也与从先进的地球观测雷诺微波扫描辐射计得出的海面温度数据集一致。诊断分析表明,海浪是海气湍流通量的附加来源,并且在增加上层海洋湍动能方面起着关键作用,从而增强了那里的温度扩散。因此,海浪也是决定台风通过时上部混合层深度的重要因素。

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