潜热通量时空变化及其趋势的贝叶斯模型研究[j]

Manoj Kumar Singh, Parvatham Venkatachalam
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引用次数: 0

摘要

本文讨论了两种模型。首先建立了潜热通量时空变异性模型,将潜热通量分解为三个周期项,即时空过程项、长期趋势项和协变量项。并提出了第二个模型来描述长期趋势及其可能的原因。两种模型均采用贝叶斯方法。所提出的方法对表征环境的时空过程变异性特别有用。采用马尔可夫链蒙特卡罗仿真技术对模型参数进行采样。这些模式用于研究1985年1月至2010年4月期间印度洋潜热通量分量。结果表明:年变异性、时空变异性和协变量变异是LHF变异性的主导因子。此外,还发现LHF的长期上升趋势主要是风速的增加。在印度洋的一些区域,海面温度的升高也是LHF增加的原因。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A Bayesian Model to Study Spatio-temporal Variability of Latent Heat Flux and its Trend

This paper talks about two models. First model is presented to study space-time variability of latent heat flux, where latent heat flux has been decomposed into three periodic terms, spatio-temporal process term, long term trend and a term due to covariates. And the second model is presented to characterize the long term trend and its possible causes. For both the models Bayesian approach was adopted. The method presented is particularly useful for characterizing environmental spatio- temporal processes variability. The model parameters were sampled using a Markov chain Monte Carlo simulation technique. The models were used for studying latent heat flux components in the Indian Ocean for the period of January 1985 to April 2010. The results showed that in LHF variability, dominant factors were annual variability, spatio-temporal variability and variability due to covariates. Further it has been found that the long term positive trend of LHF is dominated by the increase in wind speed. In some regions of Indian Ocean, increase in sea surface temperature has also been the cause for increase in LHF.

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