• Sorted by Date • Sorted by Last Name of First Author •
Wang, Dong, Tang, Bo-Hui, Li, Yingyun, Fu, Wei, Fu, Zhitao, Zhang, Zhen, and Ge, Zhongxi, 2025. GRACE-derived spatiotemporal changes of terrestrial water storage in the major plateaus of China. Global and Planetary Change, 255:105102, doi:10.1016/j.gloplacha.2025.105102.
• from the NASA Astrophysics Data System • by the DOI System •
@ARTICLE{2025GPC...25505102W,
author = {{Wang}, Dong and {Tang}, Bo-Hui and {Li}, Yingyun and {Fu}, Wei and {Fu}, Zhitao and {Zhang}, Zhen and {Ge}, Zhongxi},
title = "{GRACE-derived spatiotemporal changes of terrestrial water storage in the major plateaus of China}",
journal = {Global and Planetary Change},
keywords = {China, Plateau, GRACE, Water storage, Long-term},
year = 2025,
month = dec,
volume = {255},
eid = {105102},
pages = {105102},
abstract = "{Changes in terrestrial water storage (TWS) significantly impact water
resource regulation in the major plateaus of China (MPC).
Traditional monitoring methods are limited by high costs and
sparse site distribution, restricting large-scale and high-
resolution assessments. The Gravity Recovery and Climate
Experiment (GRACE) and its follow-on mission offer an effective
approach for TWS observation in these areas. This study examines
the spatiotemporal features of TWS in MPC from 2002 to 2022 by
recovering low-degree signals through coefficient substitution,
restoring high-degree signals via combined filtering, and
interpolating missing data using Singular Spectrum Analysis
(SSA). Key findings reveal a TWS change rate of
{\ensuremath{-}}0.1 cm/year in the MPC, with semi-annual and
annual amplitudes of 0.7 cm and 2.3 cm, respectively, peaking
between September and October. TWS variations in the MPC are
largest in the Qinghai-Tibet Plateau (QTP) and this dominant
signal tends to mask the trends in other plateau regions. Among
these, the Yunnan-Kweichow Plateau (YKP) is exhibiting a
gradually increasing TWS trend. In the western YKP, TWS declines
due to concentrated rainfall, while in its eastern regions, a
combination of reduced seasonal precipitation and water
migration contributes to an overall upward trend. These findings
provide critical insights for regional water resource management
and policy formulation.}",
doi = {10.1016/j.gloplacha.2025.105102},
adsurl = {https://ui.adsabs.harvard.edu/abs/2025GPC...25505102W},
adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}
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