• Sorted by Date • Sorted by Last Name of First Author •
Chen, Junxu, Wang, Yuan, Zhao, Zhifang, Fan, Yunjiang, Luo, Xiaochuan, Yi, Lu, Feng, Siqi, and Yang, Liang Emlyn, 2025. Natural and human-induced decline and spatio-temporal differentiation of terrestrial water storage over the Lancang-Mekong River Basin. Journal of Geographical Sciences, 35(1):112–138, doi:10.1007/s11442-025-2315-6.
• from the NASA Astrophysics Data System • by the DOI System •
@ARTICLE{2025JGSci..35..112C,
author = {{Chen}, Junxu and {Wang}, Yuan and {Zhao}, Zhifang and {Fan}, Yunjiang and {Luo}, Xiaochuan and {Yi}, Lu and {Feng}, Siqi and {Yang}, Liang Emlyn},
title = "{Natural and human-induced decline and spatio-temporal differentiation of terrestrial water storage over the Lancang-Mekong River Basin}",
journal = {Journal of Geographical Sciences},
keywords = {spatio-temporal variation, contribution separation, GRACE, Empirical Orthogonal Function, Lancang-Mekong River, Earth Sciences, Physical Geography and Environmental Geoscience},
year = 2025,
month = jan,
volume = {35},
number = {1},
pages = {112-138},
abstract = "{Due to water conflicts and allocation in the Lancang-Mekong River Basin
(LMRB), the spatio-temporal differentiation of total water
resources and the natural-human influence need to be clarified.
This work investigated LMRB's terrestrial water storage anomaly
(TWSA) and its spatio-temporal dynamics during
2002{\textendash}2020. Considering the effects of natural
factors and human activities, the respective contributions of
climate variability and human activities to terrestrial water
storage change (TWSC) were separated. Results showed that: (1)
LMRB's TWSA decreased by 0.3158 cm/a. (2) TWSA showed a gradual
increase in distribution from southwest of MRB to middle LMRB
and from northeast of LRB to middle LMRB. TWSA positively
changed in Myanmar while slightly changed in Laos and China. It
negatively changed in Vietnam, Thailand and Cambodia. (3) TWSA
components decreased in a descending order of soil moisture,
groundwater and precipitation. (4) Natural factors had a
substantial and spatial differentiated influence on TWSA over
the LMRB. (5) Climate variability contributed 79\% of TWSC in
the LMRB while human activities contributed 21\% with an
increasing impact after 2008. The TWSC of upstream basin
countries was found to be controlled by climate variability
while Vietnam and Cambodia's TWSC has been controlled by human
activities since 2012.}",
doi = {10.1007/s11442-025-2315-6},
adsurl = {https://ui.adsabs.harvard.edu/abs/2025JGSci..35..112C},
adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}
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