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首页> 外文期刊>The Open Atmospheric Science Journal >Effects of Orography on the Tail-End Effects of Typhoon Ketsana
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Effects of Orography on the Tail-End Effects of Typhoon Ketsana

机译:地形对台风凯萨娜尾巴效应的影响

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The study of tail-end effects of typhoon on orography is new to Malaysia. The current study used FY-2Dsatellite data to investigate the variation of selected parameters of the Typhoon Ketsana system. In situ data, obtained viathe radiosonde technique, were used to verify the atmospheric conditions, whereas the Advanced Spaceborne ThermalEmission and Reflection Radiometer Global Digital Elevation Model was applied to determine the structure of themountains in East Malaysia (EM). This study aimed to identify typhoon-terrain effects, in terms of wind, cloud, and rainof the tail-end effects of typhoon in a regional environment. The tail-end effects of Typhoon Ketsana were altered by theorography in EM such that a slow movement with higher rate of rainfall was distributed along the mountainous westernregion, and cloud classification distribution patterns were different before, during, and after the tail-end effects of thetyphoon. The wind intensity increased with altitude and affected the larger atmosphere region over EM. Additionally, thelocation of the Sabah region puts it at a higher risk to the impact of the tail-end effect of typhoons compared with theSarawak region due to its distance from the typhoon. This study concluded that the impacts of the tail-end effects of atyphoon can also be varied and enhanced by the orography.
机译:台风对地形的末端效应的研究对马来西亚来说是新的。当前的研究使用FY-2D卫星数据来研究台风Ketsana系统所选参数的变化。通过无线电探空仪技术获得的原位数据用于验证大气条件,而先进的星载热发射和反射辐射计全球数字高程模型则用于确定东马来西亚(EM)的山峰结构。本研究旨在根据区域环境中台风尾部效应的风,云和雨来确定台风地形效应。 EM的理论改变了台风凯萨娜的尾端效应,使得降雨速率较高的缓慢运动分布在西部山区,且前后的云分布方式有所不同。台风。风强度随着海拔的升高而增加,并影响了整个EM的更大的大气区域。此外,沙巴地区的位置使它受台风尾端效应影响的风险比沙捞越地区高,因为它距台风较远。这项研究得出的结论是,地形也可以改变和增强台风尾部效应的影响。

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