利用有限气候资料和贝叶斯模式平均估算参考蒸散量

S. Hernández, L. Morales, P. Sallis
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引用次数: 8

摘要

由于用于环境和天气监测的传感器和传感器网络数量的增加,我们提出了一种从有限气候数据中估计参考蒸散发(\ET0)的方法。对粮农组织标准Penman-Monteith方程(\PM)进行了若干修改,使我们能够使用有限的气候数据来估计\ET0,但是这些方程必须根据不同的气候条件进行局部调整。在本文中,我们使用贝叶斯模型平均来确定解释\ET0的不同模型的不确定性。利用这种方法,我们结合多个回归模型来解决气候变量的多重共线性问题。更具体地说,我们将\ET0\的估计视为一个非平稳回归问题,其中控制平均值和噪声过程的规则可能会根据不同的气候条件而变化。为了建立候选模型,我们使用了一种被称为树高斯过程(TGP)的分而治之方法,然后通过使用由\PM\方程计算的\ET0\时间序列来演示该方法。结果还与其他回归技术和计算\ET0的简化方程进行了比较。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Estimation of Reference Evapotranspiration Using Limited Climatic Data and Bayesian Model Averaging
Motivated by the increased number of sensors and sensor networks for environmental and weather monitoring, we propose a method to estimate reference evapotranspiration (\ET0) from limited climate data. There are several modifications to the standard FAO Penman-Monteith equation (\PM) that enables us to use limited climatic data for estimating \ET0, however these equations have to be adjusted locally depending of the different climatic conditions. In this paper, we use Bayesian model averaging in order to determine the uncertainty of different models that explain \ET0. Using this approach, we tackle the multi-collinearity problem of climatic variables by combining multiple regression models. More specifically, we consider estimation of \ET0\, as a non-stationary regression problem where the rules governing the mean and noise processes might change depending of the different climatic conditions. In order to build the candidate models, we use a divide and conquer approach known as Treed Gaussian Processes (TGP) and then demonstrate the method by using time series of \ET0\ calculated by means of the \PM\, equation. The results are also compared with other regression techniques and simplified equations for calculating \ET0.
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