基于机器学习的月度和季节性密歇根州降雪统计建模:多尺度方法

Lei Meng, Laiyin Zhu
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引用次数: 0

摘要

雪是地球气候系统的重要组成部分,降雪强度和变化往往对社会、环境和生态系统产生重大影响。由于在不同时空尺度上存在多种控制机制,了解月和季节降雪强度及其变化具有挑战性。利用65年的现场降雪观测,基于选定的环境和气候变量,我们评估了7种机器学习算法,用于模拟密歇根下半岛(LPM)的月度和季节性降雪。结果表明,贝叶斯加性回归树(BART)对月平均降雪量的拟合效果(R2 = 0.88)和样本外估计效果(R2 = 0.58)最好,其次是随机森林模型。BART还展示了对每月大降雪量的强大估计能力。BART和Random Forest模型均表明,地形、局地/区域环境因子和遥相关指数可以显著改善LPM的月和季节降雪量估算。这些基于机器学习算法的统计模型可以包含多个尺度的变量,并解决降雪变化对环境/气候变化的非线性响应。结果表明,多尺度机器学习技术为模拟降雪强度和变率提供了一种可靠且计算效率高的方法。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Statistical modeling of monthly and seasonal Michigan snowfall based on machine learning: A multiscale approach
Snow is an important component of Earth’s climate system and snowfall intensity and variation often significantly impact society, the environment, and ecosystems. Understanding monthly and seasonal snowfall intensity and variations is challenging because of multiple controlling mechanisms at different spatial and temporal scales. Using a 65-year of in-situ snowfall observation, we evaluated seven machine learning algorithms for modeling monthly and seasonal snowfall in the Lower Peninsula of Michigan (LPM) based on selected environmental and climatic variables. Our results show that the Bayesian Additive Regression Trees (BART) has the best fitting (R2 = 0.88) and out-of-sample estimation skills (R2 = 0.58) for the monthly mean snowfall followed by the Random Forest model. The BART also demonstrates strong estimation skills for large monthly snowfall amounts. Both BART and the Random Forest models suggest that topography, local/regional environmental factors, and teleconnection indices can significantly improve the estimation of monthly and seasonal snowfall amounts in the LPM. These statistical models based on machine learning algorithms can incorporate variables at multiple scales and address nonlinear responses of snowfall variations to environmental/climatic changes. It demonstrated that the multiscale machine learning techniques provide a reliable and computationally efficient approach to modeling snowfall intensity and variability.
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