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Numerical Study of Topographic Effect on Rainfall Reinforcement Associated with Tropical Cyclone Talim (2005)

机译:热带气旋塔里姆与热带气旋塔里姆(2005)有关的地形效果的数值研究(2005)

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@@ 1. Introduction Observational evidence (Chen and Ding, 1979; Tao et al.. 1980; Chen, 2007) has shown that tropical cyclones (TC) often bring about torrential rains when they make landfall. When a TC weakens into a remnant, rainfall would be decreased correspondingly. Howe'ver, in some cases, the remnant will be reviviscent and produce even heavier rainfall than it in landfall time. Such a phenomenon is known as Rainfall Reinforcement associated with Landfalling Tropical Cyclones (RRLTC; Fan et al., 1996). Because of the occurrence of RRLTC often under complex atmospheric environments, the prediction of RRLTC has always been a challenge to forecasters. As a result, it may induce tremendous disasters. Statistical research reveals that rainfall centers have a close relation with topography as mainly locating in coastal lines vicinity, the eastem and southem slopes of the Mountains (Dong et al., 2010). Typhoon Talim (2005) is a good case to investigate topographic effect on the rainfall reinforcement, which induced the strongest rainfall reinforcement so far in China and the rainfall center just situates in the east slope of Da-bie Mountains. In this paper, we will present results from simulation to understand the terrain impact.
机译:@@ 1.简介观察证据(陈和丁,1979; Tao等人1980;陈,2007)表明热带旋风(Tc)经常带来登陆时的暴雨。当TC削弱到残余物时,降雨将相应地减少。在某些情况下,Howe'ver在某些情况下,残余将是恢复生成的,并且在登陆时间内产生较重的降雨。这种现象称为与登陆热带气旋相关的降雨增强(RRLTC; FAN等人,1996)。由于RRLTC经常发生在复杂的大气环境下,RRLTC的预测一直是对预报员的挑战。结果,它可能会引起巨大的灾难。统计研究表明,降雨中心与主要定位在沿海地区附近,山脉的EASTEM和SOUTHEM山坡上的地形相关联系(Dong等,2010)。 Typhoon Talim(2005)是一个良好的案例,可以调查对降雨加固的地形影响,这在中国迄今为止最强大的降雨增强以及降雨中心只是在大冰山的东坡。在本文中,我们将从模拟中提出结果以了解地形影响。

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