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Chen, Zhiwei, Zhang, Xingfu, and Chen, Jianhua, 2021. Monitoring Terrestrial Water Storage Changes with the Tongji-Grace2018 Model in the Nine Major River Basins of the Chinese Mainland. Remote Sensing, 13(9):1851, doi:10.3390/rs13091851.
• from the NASA Astrophysics Data System • by the DOI System •
@ARTICLE{2021RemS...13.1851C,
author = {{Chen}, Zhiwei and {Zhang}, Xingfu and {Chen}, Jianhua},
title = "{Monitoring Terrestrial Water Storage Changes with the Tongji-Grace2018 Model in the Nine Major River Basins of the Chinese Mainland}",
journal = {Remote Sensing},
keywords = {GRACE, terrestrial hydrology, groundwater storage, the nine major river basins of Chinese mainland, in situ observations},
year = 2021,
month = may,
volume = {13},
number = {9},
eid = {1851},
pages = {1851},
abstract = "{Data from the Gravity Recovery and Climate Experiment (GRACE) satellite
mission can be used to monitor changes in terrestrial water
storage (TWS). In this study, we exploit the TWS observations
from a new temporal gravity field model, Tongji-Grace2018, which
was developed using an optimized short-arc approach at Tongji
University. We analyzed the changes in the TWS and groundwater
storage (GWS) in each of the nine major river basins of the
Chinese mainland from April 2002 to August 2016, using Tongji-
Grace2018, the Global Land Data Assimilation System (GLDAS)
hydrological model, in situ observations, and additional
auxiliary data (such as precipitation and temperature). Our
results indicate that the TWS of the Songliao, Yangtze, Pearl,
and Southeastern River Basins are all increasing, with the most
drastic TWS growth occurring in the Southeastern River Basin.
The TWS of the Yellow, Haihe, Huaihe, and Southwestern River
Basins are all decreasing, with the most drastic TWS loss
occurring in the Haihe River Basin. The Continental River Basin
TWS has remained largely unchanged over time. With the exception
of the Songliao and Pearl River Basins, the GWS results produced
by the Tongji-Grace2018 model are consistent with the in situ
observations of these basins. The correlation coefficients for
the Tongji-Grace2018 model results and the in situ observations
for the Yellow, Huaihe, Yangtze, Southwestern, and Continental
River Basins are higher than 0.710. Overall, the GWS results for
the Songliao, Yellow, Haihe, Huaihe, Southwestern, and
Continental River Basins all exhibit a downward trend, with the
most severe groundwater loss occurring in the Haihe and Huaihe
River Basins. However, the Yangtze and Southeastern River Basins
both have upward-trending modeled and measured GWS values. This
study demonstrates the effectiveness of the Tongji-Grace2018
model for the reliable estimation of TWS and GWS changes on the
Chinese mainland, and may contribute to the management of
available water resources.}",
doi = {10.3390/rs13091851},
adsurl = {https://ui.adsabs.harvard.edu/abs/2021RemS...13.1851C},
adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}
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