高分辨率全球非流体静力模式下热带气旋活动和结构对全球变暖的响应

Y. Yamada, M. Satoh, M. Sugi, C. Kodama, A. Noda, M. Nakano, T. Nasuno
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引用次数: 87

摘要

摘要利用14km网格气候模拟的输出,研究了热带气旋活动和结构的未来变化。在当前和较暖的气候条件下,采用非流体静力二十面体大气模式对对流进行了一组30年的模拟。模型预测,在气候变暖条件下,全球TC频率减少22.7%,强TC比例增加6.6%,TC中心100 km内降水率增加11.8%。这些趋势与以往采用流体静力全局模式进行积云参数化的研究结果一致。研究了具有相同强度类别的tc垂直和水平结构对全球变暖的响应。对于最低海平面气压(SLP)小于980 hPa的tc,模型预测眼壁外区域的切向风增加。切向风的增加与风速有关。
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Response of tropical cyclone activity and structure to a global warming in a high-resolution global nonhydrostatic model
AbstractWe investigated future changes in tropical cyclone (TC) activity and structure using the outputs of a 14-km mesh climate simulation. A set of 30-year simulations were performed under present-day and warmer climate conditions using a nonhydrostatic icosahedral atmospheric model with explicitly calculated convection. The model projected that the global frequency of TCs is reduced by 22.7%, the ratio of intense TCs is increased by 6.6%, and the precipitation rate within 100 km of the TC center increased by 11.8% under warmer climate conditions. These tendencies are consistent with previous studies using hydrostatic global model with cumulus parameterization.The responses of vertical and horizontal structures to global warming are investigated for TCs with the same intensity categories. For TCs whose minimum sea-level pressure (SLP) reaches less than 980 hPa, the model predicted that tangential wind increases in the outside region of the eyewall. Increases in the tangential wind are related to the ele...
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