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Modulation of winter precipitation associated with tropical cyclone of the western North Pacific by the stratospheric Quasi-Biennial oscillation

机译:北北太平洋冬季沉淀的调节北北太平洋与地梯拟两年两年两年 - 两年两年振荡

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摘要

Tropical cyclone precipitation (TCP) has increasing impacts on many coastal regions under global warming. Causes of TCP variation have been principally explored in the troposphere. This study identifies the significant modulation of the stratosphere Quasi-Biennial oscillation (QBO) on the winter TCP in the coastal regions of the western North Pacific (WNP). In the westerly QBO winter, the zonal wind vertical shear anomalies in the stratosphere strengthen (weaken) convective activities around the East China Sea (the Philippines) and cause middle-level easterly (westerly) anomalies of the middle (low) latitudes in the troposphere, leading to more (less) TC activities around the East China Sea (the Philippines). Consequently, a TCP dipole pattern can be observed. The TCP increases in East China, Korean peninsula, Japan and Russian Far East, but decreases in Indo-China Peninsula, South China and the Philippines. These results not only improve the knowledge of QBO-TCP relationship but also provide a potential indicator for the seasonal prediction of the TCP in the coastal regions of the WNP due to the high predictability of the QBO.
机译:在全球变暖的情况下,热带气旋降水(TCP)对许多沿海地区的影响越来越大。TCP变化的原因主要在对流层中进行了探索。本研究确定了平流层准两年振荡(QBO)对北太平洋西部沿海地区冬季TCP的显著调制。在西风QBO冬季,平流层的纬向风垂直切变异常加强(减弱)东海(菲律宾)周围的对流活动,并导致对流层中(低)纬的中层偏东(西风)异常,导致东海(菲律宾)周围的TC活动更多(更少)。因此,可以观察到TCP偶极子模式。中国东部、朝鲜半岛、日本和俄罗斯远东地区的TCP增加,但印度支那半岛、华南和菲律宾的TCP减少。这些结果不仅提高了对QBO-TCP关系的认识,而且由于QBO的高度可预测性,为西太平洋沿岸地区TCP的季节性预测提供了一个潜在的指标。

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