Terrestrial water storage in semi-arid basins is increasingly affected by the combined pressures of climate variability, land use change and intensive human activities. However, how landscape composition and configuration interact with climatic forcing to shape basin-scale terrestrial water storage anomalies (TWSA) remains insufficiently understood, particularly in rapidly urbanising tributary basins of the Yellow River. This study integrates GRACE/GRACE-FO-derived TWSA, meteorological observations and multi-period land use data to examine the coupled relationships among climate variability, landscape patterns and water storage in the human-dominated Yiluo River Basin. The results show that basin-averaged TWSA experienced a significant long-term decline during the GRACE/GRACE-FO period (−4.47 mm yr−1), with a statistically detectable transition around 2012 and stronger depletion in the northern and eastern parts of the basin. Precipitation exhibited a cumulative and delayed relationship with TWSA, with the strongest raw association occurring under a six-month accumulation and one-month lag (Pearson’s r = 0.44, p < 0.001, n = 134). After removing the seasonal cycle, the relationship remained significant but weaker (r = 0.30, p = 0.001, n = 129), indicating that precipitation explains part, but not all, of the interannual variability in water storage. Landscape composition showed stronger associations with TWSA than landscape configuration. Construction land was negatively associated with water storage, whereas cultivated land and grassland showed positive associations, suggesting that impervious surface expansion and the loss of permeable land may weaken the basin’s water retention capacity. These findings indicate that water storage change in the Yiluo River Basin is shaped by both climatic forcing and human-induced land surface transformation. Basin management should therefore prioritise the control of urban impervious surface expansion, the protection of permeable agricultural and ecological land, and the integration of land use planning with adaptive water resource regulation.
Climate change affects water resources in semi-arid basins by altering precipitation, land surface temperature (LST), evapotranspiration, and surface-water persistence. This study assessed hydroclimatic variability in the Lower Zab River Basin (LZRB), Iraq, during 2000–2021 using satellite and reanalysis datasets pro...
A. Al-lami, Y. Al-Timimi, A. Al-Salihi· Water Practice & Technol...· 0 citations
In cold and arid regions, climate change has altered precipitation patterns and accelerated glacierized retreat, which imposes severe risks on the stability of regional hydrological systems. Combined with the strong interactions between surface water (SW) and groundwater (GW) regulated by distinctive geological conditi...
Wenjun Wang, Ai-Hua Long, Jia-Wen Yu et al.· Applied Water Science· 0 citations
Water quality degradation in river ecosystems is a growing global challenge,
driven by both anthropogenic activities and climate change. The Kashafroud River
in northeastern Iran is a critical water source for nearly two million people, yet it
faces mounting pressures from rising temperatures (~1.5 °C over the past thr...
Marzieh Mohammadi Aria, A. Ghezelsofloo, Ben Jarihani· Central Asian Journal of Wat...· 0 citations
Lake area dynamics are sensitive indicators of hydroclimatic variability in cold‐arid regions. We reconstructed lake area changes across the Mongolian Plateau from 1990 to 2025 using Landsat imagery, JRC Global Surface Water, and HydroLAKES, and applied XGBoost and SHAP to examine associations with hydroclimatic, e...
Hydrological variability in river basins is strongly influenced by LULC changes, particularly in tropical regions where rapid forest transformation and agricultural expansion alter rainfall–runoff processes. Understanding how these dynamic land surface changes affect precipitation–discharge relationships is essential f...
D. Pandi, Muthukrishnavellaisamy Kumarasamy· Indonesian Journal of Geogra...· 0 citations
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