Time Series of Rainfall Model with Markov Switching Autoregressive

D. Devianto, Maiyastri, Uqwatul Alma Wisza, M. Wara, Putri Permathasari, Rika Okda Marlina Zen
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引用次数: 4

Abstract

The intensity of rainfall can sometimes change due to seasonal changes, extreme weather changes or weather effects in other areas around a particular location. The changes of rainfall can be categorized as a change in structure or condition that often occur in time series data, it be influenced by an unobserved random variable, that is called as a state. Then structural change of rainfall can be modeled by using Markov Switching Autoregressive (MSAR) as the result from merging the Markov chain and the classic Autoregressive model in the data mining analysis. Therefore, this study will determine the best model for rainfall at the specific hilly location but close to the shore of the Indian Ocean, that is Limau Manis sub-district of Padang city, this is to obtain the probability of displacement and survival of a state, and the amount of suspected duration of each state. The rainfall data are defined in two states of rainfall condition, high rainfall and low rainfall. The best model MSAR is obtained as MS(2)-AR(2) with the probability of transition from state high rainfall to high rainfall has 0.84379, state high rainfall to state low rainfall has 0.15621, state low rainfall to state low rainfall has 0.37516 and state low rainfall to state high rainfall has 0.62485. While the expected duration of high rainfall is 6.40161 months and the expected duration of low rainfall is 1.60039 months. This result confirms that the high rainfall duration is longer than the low rainfall duration which is very specific intensity of rainfall at the selected location.
马尔可夫切换自回归降雨时间序列模型
降雨强度有时会因季节变化、极端天气变化或特定地点周围其他地区的天气影响而改变。降雨的变化可以归类为经常发生在时间序列数据中的结构或状态的变化,它受到一个不可观测的随机变量的影响,称为状态。然后将马尔可夫链与经典自回归模型相结合,利用马尔可夫切换自回归模型(MSAR)对降水结构变化进行建模。因此,本研究将确定在靠近印度洋海岸的特定丘陵位置,即巴东市Limau Manis街道的最佳降雨模型,从而获得一种状态的位移和生存概率,以及每种状态的疑似持续时间。降雨数据被定义为两种降雨状态:高降雨和低降雨。最佳模型MSAR为MS(2)-AR(2),从强降水状态到强降水状态的转换概率为0.84379,强降水状态到弱降水状态的转换概率为0.15621,弱降水状态到弱降水状态的转换概率为0.37516,弱降水状态到强降水状态的转换概率为0.62485。高降水预期持续时间为6.40161个月,低降水预期持续时间为1.60039个月。这一结果证实了高降雨持续时间比低降雨持续时间更长,低降雨持续时间是所选地点非常特定的降雨强度。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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