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A quasitropical cyclone over the Black Sea: Observations and numerical simulation

机译:黑海上的一次准热带气旋:观测和数值模拟

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A long-living mesoscale cyclone observed over the Black Sea in September 2005 was characterized by a high wind velocity (25 m/sec) and induced an abnormal lowering of the sea-surface temperature (by more than 10°C). We performed the numerical simulation of this cyclone by using the MM5 model and the data of global operative analysis. The evolution of the cyclone and its structure similar to the structure of a tropical cyclone are reproduced. The primary azimuthal and secondary radial circulations, the clear-sky eye with warm core at medium levels, and the eyewall with strong air updraft and intense convection and precipitation are well visible. The fluxes of sensible and latent heat on the sea surface played the key role in the initiation and development of this cyclone.
机译:2005年9月在黑海上空观测到的一个长寿命的中尺度气旋的特征是高风速(25 m / sec)并引起海面温度异常降低(超过10°C)。我们通过使用MM5模型和整体运行分析数据对旋风分离器进行了数值模拟。复制了旋风的演变及其结构,类似于热带旋风的结构。可以清楚地看到主要的方位角和次要的径向环流,晴空的眼睛和中等水平的暖核,以及眼壁的强劲气流和强烈的对流和降水。海面的感热和潜热通量在该旋风的产生和发展中起着关键作用。

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