Analyzing the Rainfall Pattern in Honduras Through Non-Homogeneous Hidden Markov Models

Gustavo Alexis Sabillón, D. Zuanetti
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Abstract

One of the major climatic interests of the last decades has been to understand and describe the rainfall patterns of specific areas of the world as functions of other climate covariates. We do it for the historical climate monitoring data from Tegucigalpa, Honduras, using non-homogeneous hidden Markov models (NHMMs), which are dynamic models usually used to identify and predict heterogeneous regimes. For estimating the NHMM in an efficient and scalable way, we propose the stochastic Expectation-Maximization (EM) algorithm and a Bayesian method, and compare their performance in synthetic data. Although these methodologies have already been used for estimating several other statistical models, it is not the case of NHMMs which are still widely fitted by the traditional EM algorithm. We observe that, under tested conditions, the performance of the Bayesian and stochastic EM algorithms is similar and discuss their slight differences. Analyzing the Honduras rainfall data set, we identify three heterogeneous rainfall periods and select temperature and humidity as relevant covariates for explaining the dynamic relation among these periods.
用非齐次隐马尔可夫模型分析洪都拉斯降雨模式
在过去的几十年里,主要的气候兴趣之一是理解和描述世界上特定地区的降雨模式作为其他气候协变量的函数。我们对洪都拉斯特古西加尔巴的历史气候监测数据进行了分析,使用非同质隐马尔可夫模型(nhhmm),这是一种通常用于识别和预测异质状态的动态模型。为了有效和可扩展地估计NHMM,我们提出了随机期望最大化(EM)算法和贝叶斯方法,并比较了它们在合成数据中的性能。虽然这些方法已经被用于估计其他几种统计模型,但nhmm的情况并非如此,它仍然广泛地使用传统的EM算法进行拟合。我们观察到,在测试条件下,贝叶斯算法和随机EM算法的性能是相似的,并讨论了它们的细微差异。通过对洪都拉斯降雨数据集的分析,我们确定了三个非均匀降雨期,并选择温度和湿度作为相关协变量来解释这些时期之间的动态关系。
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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