• Sorted by Date • Sorted by Last Name of First Author •
Yuan, Xilong, Wang, Fengwei, Zhou, Yunqi, and Zhou, Shijian, 2026. Overcoming single model bias through GRACE and multi model data reveals Iran water storage depletion drivers. Scientific Reports, 16(1):22206, doi:10.1038/s41598-026-51961-6.
• from the NASA Astrophysics Data System • by the DOI System •
@ARTICLE{2026NatSR..1622206Y,
author = {{Yuan}, Xilong and {Wang}, Fengwei and {Zhou}, Yunqi and {Zhou}, Shijian},
title = "{Overcoming single model bias through GRACE and multi model data reveals Iran water storage depletion drivers}",
journal = {Scientific Reports},
keywords = {GRACE, Hydrological models, TWSA, Least-squares method, Linear trend, Earth Sciences, Physical Geography and Environmental Geoscience, Engineering, Environmental Engineering, Environmental Sciences, Environmental Science and Management},
year = 2026,
month = may,
volume = {16},
number = {1},
eid = {22206},
pages = {22206},
abstract = "{Rapid changes in terrestrial water storage (TWS) pose serious threats to
water security in arid and semi-arid regions such as Iran.
However, the inherent uncertainties of individual hydrological
models hinder robust assessments of the respective impacts of
natural variability and anthropogenic influence on water storage
dynamics in these areas. To address this issue, our study
integrates GRACE/GRACE-FO satellite gravity data, five
mainstream hydrological models (GLDAS-Noah, GLDAS-VIC, GLDAS-
CLSM, ERA5, and WGHM), and GPM global precipitation data. Four
observational datasets related to precipitation, runoff, and
evapotranspiration were derived, and 64 different hydrological
model combinations were constructed. These combinations were
comprehensively evaluated against Mascon products as a
benchmark. Ultimately, the model combination with the best
fitting performance was selected for spatial and temporal
variation analysis and attribution analysis. The findings reveal
that: (1) The model combination constructed using ERA5-derived
evapotranspiration and runoff data, combined with precipitation
data from VIC/CLSM, exhibits the highest consistency with Mascon
data. (2) In densely populated northern and southwestern
regions, the natural water flux shows significant upward trends.
Nevertheless, TWSA declines there because anthropogenic
extraction (captured in the net residual) outweighs the natural
increase, causing groundwater discharge to surface systems and
amplifying evapotranspiration and runoff losses. (3) In sparsely
populated arid central regions, TWSA remains relatively stable,
with an average annual natural water anomaly change rate of
approximately + 0.01 cm/yr, primarily due to the offsetting
effects of precipitation and evapotranspiration. This study
systematically evaluates the applicability of a multi-model
approach in arid regions. The integrated hydrological modeling
framework developed herein provides a methodology for selecting
model configurations and quantifying associated uncertainties in
water storage assessment, thereby offering a scientific basis
for sustainable water resource management in arid environments.}",
doi = {10.1038/s41598-026-51961-6},
adsurl = {https://ui.adsabs.harvard.edu/abs/2026NatSR..1622206Y},
adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}
Generated by
bib2html_grace.pl
(written by Patrick Riley
modified for this page by Volker Klemann) on
Mon Aug 24, 2026 17:14:25
GRACE-FO
Mon Aug 24, F. Flechtner![]()