基于燃烧区外部区域与苏门答腊南部降雨共同作用的二元分布形成分析

S. Nurdiati, M. Najib, Muhammad Zidane Bayu
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引用次数: 0

摘要

印度尼西亚的森林和土地与周围的气候条件(如降雨量)有着密切的关系。一个可以用来分析两个变量之间关系的模型是copula。然而,除了降雨之外,厄尔尼诺南方涛动(ENSO)和印度洋偶极子(IOD)等全球气候现象也会对森林和土地产生影响。因此,本研究通过基于ENSO和IOD现象的数据划分,分析和模拟了降雨和烧伤面积之间基于copula的共同分布。所使用的方法是基于copula的联合分布分析,该分析使用边际函数推断(IFM)方法进行估计。几个copula函数用于形成联合分布,如Gaussian、student's t、Clayton、Gumbel、Frank、Joe、Galambos、BB1(Clayton Gumbel)、BB6(Joe Clayton)、BB7(Joe Gumbel和BB8(Joe Frank)。结果表明,基于Kendall-Tau相关性的两个月累积降雨量数据与烧伤面积的相关性最高。每种ENSO和IOD条件都有不同的特征,通过所选单变量分布和copula函数的差异来表示。降雨量较低时,燃烧区域的可能性较高。此外,ENSO和IOD指数越高,在低降雨量期间发生燃烧区域的概率就越高。根据条件概率,正IOD条件比中等强度厄尔尼诺具有相对更大的影响。除了中等强度的厄尔尼诺和正IOD外,另一种条件概率相对较高的条件是弱厄尔尼诺条件。其他条件,如拉尼娜现象、正常ENSO、负IOD和中性IOD,具有非常小的烧伤面积的条件概率。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Analisis Pembentukan Sebaran Bivariat Berbasis Copula Antara Luas Area Terbakar dan Curah Hujan di Sumatra Bagian Selatan
Forest and land fires in Indonesia have a close relationship with the surrounding climatic conditions, such as rainfall. One model that can be used to analyze the relationship between the two variables is the copula. However, apart from rainfall, global climate phenomena such as the El Nino-Southern Oscillation (ENSO) and the Indian Ocean Dipole (IOD) also have an influence on forest and land fires. Therefore, this study analyzes and models the copula-based co-distribution between rainfall and burned area by partitioning the data based on ENSO and IOD phenomena. The method used is copula-based joint distribution analysis which is estimated using the Inference of Function for Margins (IFM) method. Several copula functions are used to form joint distributions, such as Gaussian, student’s t, Clayton, Gumbel, Frank, Joe, Galambos, BB1 (Clayton-Gumbel), BB6 (Joe-Clayton), BB7 (Joe-Gumbel), and BB8 (Joe-Frank). The results showed that the highest correlation to the burned area occurred for the two months cumulative rainfall data based on the Kendall-Tau correlation. Each ENSO and IOD condition has different characteristics, indicated by the differences in the selected univariate distribution and copula function. Probabilities of burning areas are higher when rainfall is low. In addition, the higher the ENSO and IOD indices, the higher the probability of burned area, during low rainfall. Based on the conditional probabilities, the Positive IOD condition has relatively more significant influence than the Moderate-Strong El Nino. Apart from the Moderate-Strong El Nino and Positive IOD, another condition that has a conditional probability for a relatively high is Weak El Nino conditions. Other conditions, such as La Nina, normal ENSO, negative IOD, and Neutral IOD, have a conditional probability of a very small burn area.
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