• Sorted by Date • Sorted by Last Name of First Author •
Zhang, Gangqiang, Zheng, Wei, Yin, Wenjie, and Lei, Weiwei, 2020. Improving the Resolution and Accuracy of Groundwater Level Anomalies Using the Machine Learning-Based Fusion Model in the North China Plain. Sensors, 21(1):46, doi:10.3390/s21010046.
• from the NASA Astrophysics Data System • by the DOI System •
@ARTICLE{2020Senso..21...46Z,
author = {{Zhang}, Gangqiang and {Zheng}, Wei and {Yin}, Wenjie and {Lei}, Weiwei},
title = "{Improving the Resolution and Accuracy of Groundwater Level Anomalies Using the Machine Learning-Based Fusion Model in the North China Plain}",
journal = {Sensors},
keywords = {machine learning-based fusion model, GRACE, gradient boosting decision tree, groundwater level anomalies, statistical downscaling, North China Plain},
year = 2020,
month = dec,
volume = {21},
number = {1},
eid = {46},
pages = {46},
abstract = "{The launch of GRACE satellites has provided a new avenue for studying
the terrestrial water storage anomalies (TWSA) with
unprecedented accuracy. However, the coarse spatial resolution
greatly limits its application in hydrology researches on local
scales. To overcome this limitation, this study develops a
machine learning-based fusion model to obtain high-resolution
(0.25{\textdegree}) groundwater level anomalies (GWLA) by
integrating GRACE observations in the North China Plain.
Specifically, the fusion model consists of three modules, namely
the downscaling module, the data fusion module, and the
prediction module, respectively. In terms of the downscaling
module, the GRACE-Noah model outperforms traditional data-driven
models (multiple linear regression and gradient boosting
decision tree (GBDT)) with the correlation coefficient (CC)
values from 0.24 to 0.78. With respect to the data fusion
module, the groundwater level from 12 monitoring wells is
incorporated with climate variables (precipitation, runoff, and
evapotranspiration) using the GBDT algorithm, achieving
satisfactory performance (mean values: CC: 0.97, RMSE: 1.10 m,
and MAE: 0.87 m). By merging the downscaled TWSA and fused
groundwater level based on the GBDT algorithm, the prediction
module can predict the water level in specified pixels. The
predicted groundwater level is validated against 6 in-situ
groundwater level data sets in the study area. Compare to the
downscaling module, there is a significant improvement in terms
of CC metrics, on average, from 0.43 to 0.71. This study
provides a feasible and accurate fusion model for downscaling
GRACE observations and predicting groundwater level with
improved accuracy.}",
doi = {10.3390/s21010046},
adsurl = {https://ui.adsabs.harvard.edu/abs/2020Senso..21...46Z},
adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}
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