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首页> 外文期刊>TAO: Terrastrial, atmospheric, and oceanic sciences >Impact of air-sea exchange coefficients on the structure and intensity of tropical cyclones
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Impact of air-sea exchange coefficients on the structure and intensity of tropical cyclones

机译:海洋交流系数对热带气旋结构和强度的影响

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摘要

To examine the impact of air-sea exchange coefficients on the structure and intensity of tropical cyclones, sensitivity experiments are performed using the Weather Research and Forecasting (WRF) Model. A typhoon-like idealized vortex embedded in a calm environment is simulated using combinations of three different values of air-sea momentum and enthalpy exchange coefficients. In order to investigate the clear roles of each exchange coefficient, the experiments are designed that the two exchange coefficients change independently. For example, while the enthalpy exchange coefficient varies, the momentum exchange coefficient keeps its original value and vice versa. The track and intensity of sensitivity tests are analyzed to check the validity of the experiments. Results show that the track of the idealized vortices under a calm environment remains stationary, while the intensity varies with different air-sea exchange coefficients. The results indicate that changes in storm intensity with different enthalpy exchange coefficients are mainly related to an alteration in the amount of energy input to the storm, whereas the intensity changes with different momentum exchange coefficient values mostly result from angular momentum conservation due to changes in the size of the vortex. There is little change in the net energy input to the storms when the values of the momentum exchange coefficient are changed. Calculations of the volume-integrated angular momentum at the radius of the maximum winds confirm the different intensifying mechanisms found in this study.
机译:为了检查空中海洋交换系数对热带气旋结构和强度的影响,使用天气研究和预测(WRF)模型进行敏感性实验。使用三种不同的海洋动量和焓交换系数的组合模拟嵌入在平静环境中的台风的理想化涡流。为了调查每个交换系数的明确作用,实验设计了两个交换系数的独立变化。例如,虽然焓交换系数变化,势头交换系数保持其原始值,反之亦然。分析敏感性测试的轨道和强度检查实验的有效性。结果表明,平静环境下理想化涡流的轨道仍然是静止的,而强度随着不同的空中交换系数而变化。结果表明,具有不同焓交换系数的风暴强度的变化主要与风暴的能量量的变化相关,而强度随着不同的动量交换系数值而变化主要是由于由于变化而导致的角动量保守导致涡旋的大小。当势头交换系数的值改变时,净能量输入的净能量几乎没有变化。最大风半径的体积集成角动量的计算确认了本研究中发现的不同强化机制。

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