加强墨西哥圣地亚哥河流域降水量的地质统计估算

Atmósfera Pub Date : 2024-07-05 DOI:10.20937/atm.53334
J. R. Ávila-Carrasco, Hugo Enrique Júnez-Ferreira, Graciela del Socorro Herrera
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引用次数: 0

摘要

准确的降水估算对于了解水文循环、其在特定流域规划中的应用以及异常事件预测至关重要。多元地质统计学利用地形高程和海岸线距离等相关变量来减少估算误差的不确定性。然而,湿季和旱季的不同特点要求采用特定的估算方法。在墨西哥西海岸广阔而多样的圣地亚哥河流域(SRB),精确的降水估算是一项挑战。本研究以海拔高度和海岸线距离为辅助变量,使用普通克里金法和普通克里金法评估了旱季和雨季的降水量估计值。误差指标评估结果显示,将海岸线距离作为湿润月份七月份的协变量,效果更佳,特别是在对数变换后,平均标准化误差比单变量方法提高了 17%。相反,在干燥月份(2 月),使用普通克里金法剔除离群值后,取得了最佳结果,有效地减少了平均平方误差。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Enhancing geostatistical precipitation estimations for the Santiago River basin, Mexico
Accurate precipitation estimation is crucial for understanding the hydrological cycle, its applications in basin-specific planning, and outliers event prediction. Multivariate geostatistics leverage correlated variables, such as terrain elevation and shoreline distance, to reduce estimation error uncertainty. However, the distinct characteristics of humid and dry seasons demand specific estimation approaches. Precise precipitation estimation poses a challenge in the vast and diverse Santiago River basin (SRB) along Mexico’s west coast. This study assessed precipitation estimates for dry and humid seasons using ordinary kriging and ordinary cokriging with altitude and shoreline distance as auxiliary variables. Evaluation of error metrics revealed superior results incorporating shoreline distance as a covariable in the wet month of July, especially after logarithmic transformation, yielding a 17% improvement in average standardized error compared to the univariate approach. Conversely, optimal results were achieved for the dry month (February) using ordinary kriging excluding outliers’ values, effectively reducing the average squared error.
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