A non-stationary downscaling and gap-filling approach for GRACE/GRACE-FO data under climatic and anthropogenic influences

IF 5.7 3区 环境科学与生态学 Q1 WATER RESOURCES
Seyed Mojtaba Mousavimehr, Mohammad Reza Kavianpour
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Abstract

Gravity Recovery and Climate Experiment (GRACE) and GRACE Follow-On (GRACE-FO) are being increasingly used as valuable data sources for hydrological monitoring. However, their coarse spatial resolution is considered as a limitation for regional studies, especially in areas with remarkable hydroclimate variability. In this study, a novel approach is presented for downscaling, and gap filling of terrestrial water storage (TWS) in Tehran province, Iran. Non-stationarity in the GRACE/GRACE-FO derived TWS is a significant challenge for predictive models. In this regard, the Hodrick–Prescott filter was adopted to detrend the TWS data. Afterward, several machine learning and deep learning techniques are employed for TWS prediction using Global Land Data Assimilation System and the fifth-generation ECMWF reanalysis (ERA5) datasets. The methodology is employed for bridging the gap between GRACE and GRACE-FO as well. Subsequently, the models are trained with different combinations of input variables and their performance is evaluated against the actual values. In parallel, a separate regression model based on the temporal index of the sample is developed for trend estimation and highlighting the role of anthropogenic activities. The proposed methodology is employed for bridging the gap between GRACE and GRACE-FO as well. The models with the highest accuracy are fed by input data with a spatial resolution of 0.25° × 0.25° to obtain fine-resolution TWS. Finally, the downscaled TWS derived from the predictive model is applied to calculate groundwater storage (GWS). The monthly TWS prediction results exhibit a strong correlation (CC = 0.93) and a low error (RMSE = 4.75 cm), underscoring the effectiveness of the proposed approach. TWS and GWS computations reveal rapid declines in groundwater-level prevailing by anthropogenic factors which exacerbate water crisis issues and environmental problems in the study area.

重力恢复与气候实验(GRACE)和重力恢复与气候实验后续项目(GRACE-FO)越来越多地被用作水文监测的宝贵数据源。然而,它们较低的空间分辨率被认为限制了区域研究,特别是在水文气候变异显著的地区。本研究提出了一种新方法,用于降尺度和填补伊朗德黑兰省陆地蓄水量 (TWS) 的缺口。GRACE/GRACE-FO 得出的陆地蓄水量的非稳态性是预测模型面临的一个重大挑战。为此,采用了霍德里克-普雷斯科特滤波器对 TWS 数据进行去趋势处理。随后,利用全球陆地数据同化系统和第五代 ECMWF 再分析(ERA5)数据集,采用多种机器学习和深度学习技术进行 TWS 预测。该方法还用于弥合 GRACE 和 GRACE-FO 之间的差距。随后,使用不同的输入变量组合对模型进行训练,并根据实际值对其性能进行评估。同时,还根据样本的时间指数开发了一个单独的回归模型,用于估计趋势并突出人为活动的作用。建议的方法也用于缩小 GRACE 和 GRACE-FO 之间的差距。精度最高的模型由空间分辨率为 0.25° × 0.25° 的输入数据提供,以获得精细分辨率的 TWS。最后,应用预测模型得出的降尺度 TWS 计算地下水储量(GWS)。月度 TWS 预测结果显示出较强的相关性(CC = 0.93)和较低的误差(RMSE = 4.75 厘米),凸显了建议方法的有效性。TWS 和 GWS 计算显示,人为因素导致地下水位迅速下降,加剧了研究区域的水危机问题和环境问题。
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来源期刊
Applied Water Science
Applied Water Science WATER RESOURCES-
CiteScore
9.90
自引率
3.60%
发文量
268
审稿时长
13 weeks
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