马来西亚半岛风暴事件的日概率模型

M. Bakar, N. M. Ariff, A. Jemain
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引用次数: 2

摘要

风暴事件分析(SEA)提供了一种将降雨事件定义为风暴的方法,其中每个风暴都有自己的数量和持续时间。通过模拟不同类型风暴的日概率,可以确定和研究降雨季节的开始、抵消和周期。此外,气象学领域的研究人员将能够研究降雨的动力学特征,并为未来的参考做出预测。在这项研究中,有四类风暴;短、中、长、超长风暴;是根据风暴持续时间的长短来介绍的。为马来西亚半岛的这四类风暴建立了风暴的日概率模型。利用伯努利分布和对第一傅里叶调和方程的线性回归建立了模型。从所获得的模式中发现,马来西亚半岛东部的日风暴概率表现为单峰型,降雨开始于年底并持续到明年初的概率很大。这很可能是由于每年11月至3月的东北季风季节。与此同时,马来西亚半岛其他地区的短期和中期风暴由于两个季风间季节而经历双峰循环。总的来说,这些模式表明,根据各种风暴事件概率的日模式,马来西亚半岛可以分为四个不同的区域。
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Daily Probability Model of Storm Events in Peninsular Malaysia
Storm Event Analysis (SEA) provides a method to define rainfalls events as storms where each storm has its own amount and duration. By modelling daily probability of different types of storms, the onset, offset and cycle of rainfall seasons can be determined and investigated. Furthermore, researchers from the field of meteorology will be able to study the dynamical characteristics of rainfalls and make predictions for future reference. In this study, four categories of storms; short, intermediate, long and very long storms; are introduced based on the length of storm duration. Daily probability models of storms are built for these four categories of storms in Peninsular Malaysia. The models are constructed by using Bernoulli distribution and by applying linear regression on the first Fourier harmonic equation. From the models obtained, it is found that daily probability of storms at the Eastern part of Peninsular Malaysia shows a unimodal pattern with high probability of rain beginning at the end of the year and lasting until early the next year. This is very likely due to the Northeast monsoon season which occurs from November to March every year. Meanwhile, short and intermediate storms at other regions of Peninsular Malaysia experience a bimodal cycle due to the two inter-monsoon seasons. Overall, these models indicate that Peninsular Malaysia can be divided into four distinct regions based on the daily pattern for the probability of various storm events.
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