首页> 外文期刊>Mausam: Journal of the Meteorological Department of India >Large-scale characteristics of rapidly intensifying tropical cyclones over the Bay of Bengal and a Rapid Intensification (RI) index
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Large-scale characteristics of rapidly intensifying tropical cyclones over the Bay of Bengal and a Rapid Intensification (RI) index

机译:孟加拉湾热带气旋迅速增强的大规模特征和快速指数(RI)

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A rapid intensification index (RII) is developed for tropical cyclones over the Bay of Bengal. The RII uses large-scale characteristics of tropical cyclones to estimate the probability of rapid intensification (RI) over the subsequent 24 hrs. The RI is defined as an increase of intensity 30 kt (15.4 ms~(-1)) during 24 hrs, which represents approximately the 93~(rd) percentile of 24 hrs intensity changes of tropical cyclones that developed over the Bay of Bengal during 1981-2010. It is found that 32% of all very severe cyclonic storms (VSCS) and all super cyclonic storms (SUCS) underwent RI phase at least once during their lifetime. Various large-scale variables associated with the RI cases are compared to those of non-RI cases. These comparisons show that the RI cases generally occur at higher latitude and are intensifying at a faster rate during the previous 12 hrs than the non-RI cases. The statistical analysis also shows that the RI cases are embedded in regions where the upper-level divergence, lower-level relative vorticity and relative humidity are more and vertical winds shear is less than certain threshold values of the respective variables. Finally, the initial wind speed of RI cases is higher and tends to move with a faster translational speed than the non-RI cases. The RII technique is developed by combining threshold (index) values of the eight variables for which statistically significant differences are found between the RI and non-RI cases. The probability of RI is found to be increases from 0% to 100% when the total number of indices satisfied increases from zero to eight.
机译:为孟加拉湾上空的热带气旋开发了一个快速强化指数(RII)。 RII利用热带气旋的大规模特征来估算随后24小时内快速集约化(RI)的可能性。 RI定义为在24小时内强度增加30 kt(15.4 ms〜(-1)),大约代表在孟加拉湾上空发展的热带气旋在24小时内强度变化的93〜(rd)百分位。 1981-2010年。已发现,在所有非常严重的气旋风暴(VSCS)和所有超级气旋风暴(SUCS)中,有32%的生命周期至少经历了一次RI阶段。将与RI案例相关的各种大规模变量与非RI案例的变量进行比较。这些比较表明,与非RI案例相比,RI案例通常发生在较高的纬度上,并且在过去的12小时内以更快的速度增强。统计分析还表明,RI案例被嵌入在上层差异较大,下层相对涡度和相对湿度较大且垂直风切变小于各个变量的特定阈值的区域。最后,RI案例的初始风速较高,并且倾向于以比非RI案例更快的平移速度移动。通过组合八个变量的阈值(索引)值来开发RII技术,对于这些变量,在RI和非RI案例之间发现了统计学上的显着差异。当满足的索引总数从零增加到八时,发现RI的概率从0%增加到100%。

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