Spatial distribution of deficit and surplus of water and its interplay with landscape relief units in the high-Andean Huancané River Basin, Puno, Peru DOI
Elmer Calizaya, Osmar Cuentas Toledo,

Melvin Pozo

et al.

Modeling Earth Systems and Environment, Journal Year: 2024, Volume and Issue: 11(1)

Published: Dec. 23, 2024

Language: Английский

Effects of the freeze–thaw process on sources and pathways of subsurface flow in an alpine hillslope on the northeastern Qinghai-Tibet Plateau DOI
Yangyang Zhang, Xiaoyan Li, Guangrong Hu

et al.

Journal of Hydrology, Journal Year: 2024, Volume and Issue: 636, P. 131291 - 131291

Published: May 10, 2024

Language: Английский

Citations

4
Surface and subsurface flow of a glacierised catchment in the cold-arid region of Ladakh, Trans-Himalaya DOI Creative Commons

Mohd Soheb,

Peter Bastian,

Susanne Schmidt

et al.

Journal of Hydrology, Journal Year: 2024, Volume and Issue: 635, P. 131063 - 131063

Published: March 11, 2024

Hydrological assessments of high-altitude catchments in Trans-Himalayan Ladakh are necessary for a better understanding water availability the context irrigated cultivation under conditions insufficient quantitative information on cryospheric meltwater discharge. In this study, an integrated spatially distributed temperature index model and coupled surface/subsurface flow were used to simulate daily, seasonal, annual surface subsurface flows assess proportion corresponding source contributors from Stok catchment. Snow glacier discharge secures agriculture more than 300 households The models forced by temperature, precipitation, ice- snow-covered areas at daily time steps with calibration (2019; 108 days) validation (2018; 93 against observed simulated shows good agreement R2 RMSE 0.8 (p < 0.01) 0.6 m3/s, respectively. results between 2003 2019 show that snowmelt contribution total is largest 65 %, followed melt rainfall contributions approximately 19 % 16 A reduction glacierised 4.2 was while showed high inter-annual variation. Simulated makes up 62 (mean = 37.2 × 106 m3) less simulation suggests ceases during winter period peaks August, annualized mean amounts ∼23.7 m3. More 50 occurs summer months June, July when intensity snowmelt, ice melt, reach its maximum. findings study important village local scale, it might also help understand socio-hydrological dynamics situations scarcity wider cold-arid region Ladakh.

Language: Английский

Citations

1
Seasonal freeze–thaw front dynamics and effects on hydrothermal processes in diverse alpine grasslands on the northeastern Qinghai–Tibet Plateau DOI
Fenglin Zuo, Xiaoyan Li, Yangyang Zhang

et al.

Journal of Hydrology, Journal Year: 2024, Volume and Issue: unknown, P. 132301 - 132301

Published: Nov. 1, 2024

Language: Английский

Citations

1
Spatiotemporal variability of dissolved carbon and sources of dissolved inorganic carbon influenced by freeze–thaw and subsurface flow in an alpine headwater catchment of the Qinghai-Tibetan Plateau DOI
Yangyang Zhang, Xiaoyan Li, Fangzhong Shi

et al.

Journal of Hydrology, Journal Year: 2024, Volume and Issue: 640, P. 131740 - 131740

Published: July 31, 2024

Language: Английский

Citations

0
Spatial distribution of deficit and surplus of water and its interplay with landscape relief units in the high-Andean Huancané River Basin, Puno, Peru DOI
Elmer Calizaya, Osmar Cuentas Toledo,

Melvin Pozo

et al.

Modeling Earth Systems and Environment, Journal Year: 2024, Volume and Issue: 11(1)

Published: Dec. 23, 2024

Language: Английский

Citations

0