Comparison features importance for temporal and spatial-temporal approaches in GRACE and GRACE-FO signal reconstruction based on GLDAS data

Pub Date : 2023-01-01 DOI:10.1504/ijhst.2023.134623
Viktor Szabó
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Abstract

Machine learning algorithms can effectively learn the complex relationships between various input variables from the global land data assimilation system (GLDAS) and the total water storage (TWS) observed by gravity recovery and climate experiment (GRACE) and GRACE-FO (follow-on) missions. As the TWS depends on various features, a serious question arises about the importance of used variables for reconstruction. Furthermore, will the variables used for the reconstruction be equally significant for grid-based and basin-based analyses? This work examined the importance of individual predictors for the temporal and spatial-temporal approach over 254 river basins using GRACE and GRACE-FO data as target and GLDAS data as predictors. The extreme gradient boosting (XGBoost) algorithm was used to reconstruct TWS. Results were evaluated with root-mean-square error, normalised root-mean-square error, Pearson correlation coefficient, Nash-Sutcliffe efficiency, and Kolmogorov-Smirnow-test metrics. Model output influence was checked by the model-agnostic version of the feature importance and by Shapley additive explanations (SHAP).
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比较了基于GLDAS数据的GRACE和GRACE- fo信号重构中时间和时空方法的重要性
机器学习算法可以有效地学习来自全球陆地数据同化系统(GLDAS)的各种输入变量与重力恢复与气候实验(GRACE)和GRACE- fo(后续)任务观测到的总储水量(TWS)之间的复杂关系。由于TWS取决于各种特征,因此出现了一个严重的问题,即用于重建的变量的重要性。此外,用于重建的变量对于基于网格和基于盆地的分析是否同样重要?本研究以GRACE和GRACE- fo数据为目标,GLDAS数据为预测因子,考察了254个流域的个体预测因子在时空方法中的重要性。采用极限梯度增强(XGBoost)算法重构TWS。采用均方根误差、归一化均方根误差、Pearson相关系数、Nash-Sutcliffe效率和kolmogorov - smirnow检验指标对结果进行评价。模型输出影响通过特征重要性的模型不可知版本和Shapley加性解释(SHAP)进行检查。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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