Multiple temporal scale variation characteristics and driving factors of arid inland runoff: A case study of Urumqi River, China

Journal of Hydrology Regional Studies, Год журнала: 2025, Номер 58, С. 102298 - 102298

Опубликована: Март 5, 2025

Язык: Английский

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The Response of the Water Cycle to landscape configuration and composition in two Chilean Basins.

Environmental and Sustainability Indicators, Год журнала: 2025, Номер unknown, С. 100629 - 100629

Опубликована: Фев. 1, 2025

Язык: Английский

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Soil water balance in response to rainfall variability over a dammed valley farmland in the Chinese Loess Plateau

Ecological Indicators, Год журнала: 2025, Номер 175, С. 113594 - 113594

Опубликована: Май 15, 2025

Язык: Английский

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Deep percolation and soil water dynamics under different sand-fixing vegetation types in two different precipitation regions in semiarid sandy Land, Northern China

Agricultural and Forest Meteorology, Год журнала: 2025, Номер 364, С. 110455 - 110455

Опубликована: Фев. 18, 2025

Язык: Английский

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A comprehensive analysis of seasonal and interannual ecohydrological process dynamics in semi-arid dune and meadow ecosystems

Journal of Hydrology, Год журнала: 2025, Номер unknown, С. 133587 - 133587

Опубликована: Май 1, 2025

Язык: Английский

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Stable isotopes reveal soil evaporation and its controlling factors in the Heihe River source area on the northeastern Qinghai-Tibetan Plateau

Journal of Hydrology Regional Studies, Год журнала: 2024, Номер 54, С. 101901 - 101901

Опубликована: Июль 29, 2024

The Heihe River source area in the Northeastern Qinghai-Tibetan Plateau, China. Soil evaporation, which is a key process soil water loss, influenced by various environmental factors. However, identification of its main drivers on large scale alpine mountains remains challenging due to sampling constraints. This study examined spatial distribution evaporation and control factors during growing season area. results indicated that represented lc-excess values, gradually increased from southeast northwest, then decreased, reaching depth 50 cm below surface. Although normalized difference vegetation index explained 54 % variation interaction between land surface temperature content (SWC) provided more robust explanation. losses exhibited following pattern: cropland > grassland forest shrubland. In shrubland, SWC precipitation 68 73.3 variations respectively. Grassland mainly relied SWC, with 49.33 unexplained variability Meanwhile, aridity aspect 45 44.6 cropland. These findings invaluable information for advancing our understanding ecohydrological processes mountains.

Язык: Английский

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Different responses of soil water to warming controlled by evapotranspiration during grassland degradation: A case study in the typical steppe of China

Ecological Indicators, Год журнала: 2024, Номер 167, С. 112718 - 112718

Опубликована: Окт. 1, 2024

Язык: Английский

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Regulating and remolding of soil water flux by sparse shrubs in arid desert regions

CATENA, Год журнала: 2024, Номер 245, С. 108285 - 108285

Опубликована: Авг. 10, 2024

Язык: Английский

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The differential responses of gas exchange and evapotranspiration to experimental drought for seedlings of two typical tree species on the Loess Plateau

Ecological Indicators, Год журнала: 2024, Номер 167, С. 112721 - 112721

Опубликована: Окт. 1, 2024

Язык: Английский

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Coupled simulation of percolation and evapotranspiration in semi-mobile and semi-fixed dunes

Journal of Hydrology, Год журнала: 2024, Номер unknown, С. 132158 - 132158

Опубликована: Окт. 1, 2024

Язык: Английский

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