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贝叶斯计算用于 delta-lognormal 分布的共同变异系数,应用于泰国的共同降雨离散度。

Bayesian computation for the common coefficient of variation of delta-lognormal distributions with application to common rainfall dispersion in Thailand.

机构信息

Department of Applied Statistics, King Mongkut's University of Technology North Bangkok, Bangkok, Thailand.

出版信息

PeerJ. 2022 Feb 4;10:e12858. doi: 10.7717/peerj.12858. eCollection 2022.

DOI:10.7717/peerj.12858
PMID:35186465
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC8820225/
Abstract

Rainfall fluctuation makes precipitation and flood prediction difficult. The coefficient of variation can be used to measure rainfall dispersion to produce information for predicting future rainfall, thereby mitigating future disasters. Rainfall data usually consist of positive and true zero values that correspond to a delta-lognormal distribution. Therefore, the coefficient of variation of delta-lognormal distribution is appropriate to measure the rainfall dispersion more than lognormal distribution. In particular, the measurement of the dispersion of precipitation from several areas can be determined by measuring the common coefficient of variation in the rainfall from those areas together. Herein, we compose confidence intervals for the common coefficient of variation of delta-lognormal distributions by employing the fiducial generalized confidence interval, equal-tailed Bayesian credible intervals incorporating the independent Jeffreys or uniform priors, and the method of variance estimates recovery. A combination of the coverage probabilities and expected lengths of the proposed methods obtained a Monte Carlo simulation study were used to compare their performances. The results show that the equal-tailed Bayesian based on the independent Jeffreys prior was suitable. In addition, it can be used the equal-tailed Bayesian based on the uniform prior as an alternative. The efficacies of the proposed confidence intervals are demonstrated applying them to analyze daily rainfall datasets from Nan, Thailand.

摘要

降雨波动使得降水和洪水预测变得困难。变异系数可用于衡量降雨的离散程度,从而提供预测未来降雨的信息,进而减轻未来的灾害。降雨数据通常包括对应于 delta-log 正态分布的正和真实零值。因此,变异系数更适合衡量 delta-log 正态分布的降雨离散程度,而不是对数正态分布。特别是,通过测量这些地区的降雨量的共同变异系数,可以确定来自几个地区的降水的离散程度。在这里,我们通过使用基于置信区间的广义置信区间、包含独立杰弗里斯或均匀先验的等尾贝叶斯可信区间,以及方差估计恢复的方法,来构建 delta-log 正态分布的共同变异系数的置信区间。通过使用蒙特卡罗模拟研究来组合这些方法的覆盖率概率和预期长度,以比较它们的性能。结果表明,基于独立杰弗里斯先验的等尾贝叶斯方法是合适的。此外,还可以使用基于均匀先验的等尾贝叶斯作为替代方法。通过应用这些方法分析来自泰国南那的每日降雨数据集,证明了所提出的置信区间的有效性。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/82d3/8820225/fc51889db4ff/peerj-10-12858-g008.jpg
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https://cdn.ncbi.nlm.nih.gov/pmc/blobs/82d3/8820225/6acf05000f50/peerj-10-12858-g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/82d3/8820225/9c5f7f4158cc/peerj-10-12858-g007.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/82d3/8820225/fc51889db4ff/peerj-10-12858-g008.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/82d3/8820225/c9a2fa11da8d/peerj-10-12858-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/82d3/8820225/3dc06cf2ca4d/peerj-10-12858-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/82d3/8820225/4d3d14ed7aee/peerj-10-12858-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/82d3/8820225/99e3fe1ea590/peerj-10-12858-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/82d3/8820225/75e05922b2fa/peerj-10-12858-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/82d3/8820225/6acf05000f50/peerj-10-12858-g006.jpg
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https://cdn.ncbi.nlm.nih.gov/pmc/blobs/82d3/8820225/fc51889db4ff/peerj-10-12858-g008.jpg

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PeerJ. 2020 Sep 21;8:e10004. doi: 10.7717/peerj.10004. eCollection 2020.
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The Bayesian confidence intervals for measuring the difference between dispersions of rainfall in Thailand.用于测量泰国降雨量离散度差异的贝叶斯置信区间。
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