初夏雨季台湾地区低空急流及其在强降雨中的作用

Yi-Leng Chen, Chuan-Chi Tu, Feng Hsiao, Ching-Sen Chen, P. Lin, P. Lin
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引用次数: 2

摘要

初夏雨季,台湾地区观测到三种类型的低空急流,包括位于锋面区850-700 hPa层的天气性低空急流(SLLJ)、位于南海北部西南季风流内约925 hPa的海相边界层急流(MBLJ),以及位于台湾西北海岸约1 km高度的地形诱导急流(如障壁急流(BJ))。综述了这三种低空急流的形成特征和物理过程,并讨论了它们在强降水过程中的作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
An Overview of Low-Level Jets (LLJs) and Their Roles in Heavy Rainfall over the Taiwan Area during the Early Summer Rainy Season
During the early summer rainy season over Taiwan, three types of low-level jets are observed, including a synoptic low-level jet (SLLJ) situated in the 850–700 hPa layer in the frontal zone, a marine boundary layer jet (MBLJ) embedded within the southwesterly monsoon flow over the northern South China Sea at approximately the 925 hPa level, and an orographically induced jet at approximately the 1 km level off the northwestern Taiwan coast (e.g., barrier jet (BJ)). The characteristics and physical processes of the formation of these three types of low-level jets are reviewed, and their roles in the development of heavy rainfall are discussed.
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