Hydrological Dimension of Ladakh under Changing Climate
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Keywords:
Glacier hydrology, snow hydrology, spring hydrology, river hydrology, climate dynamics in Ladakh, cryosphere–hydrology interactions, trans- Himalayan region, water securityAbstract
Ladakh, in the Trans-Himalayan region of northern India, hosts a distinctive high-altitude cold-arid hydrological system in which seasonal snow, glaciers, perched aquifers and a limited network of perennial rivers jointly determine water availability for ecological and human systems. This narrative review-synthesis combines literature analysis (80+ studies) with original trend assessment of IMD gridded rainfall/temperature data (1975–2024) using Modified Mann-Kendall tests and Sen’s slope estimation to comprehend the changes in climate and hydrological dimensions. The synthesis reveals significant warming (+0.02°C yr-1, p<0.05) across Ladakh with spatially variable precipitation trends, earlier snowmelt timing (∼1.2 days yr −1), and glacier mass loss (−0.21 to −0.37 m w.e. yr-¹). Springs show declining perennial discharge while Indus tributaries maintain 62–72% cryospheric runoff contribution. Springs and shallow groundwater systems provide disproportionately important perennial supply where surface waters are strongly seasonal, and precipitation is sparse, and major rivers (notably the upper Indus and tributaries such as the Suru, Zanskar, Shyok, and Nubra) integrate cryospheric and groundwater signals at basin scales. Observational and modelling evidence indicate a system in warming drives earlier snowmelt and a transient increase in glacier runoff, followed by long-term declines in glacier melt contributions as ice volume diminishes; concomitant shifts in recharge reduce spring resilience and alter river seasonality. These dynamics increase exposure to both chronic water scarcity and abrupt hazards. To manage these interconnected risks, we recommend priorities: establishment of integrated high-altitude monitoring networks for snow, ice, springs, and river discharge; process-based modelling that couples downscaled climate projections with cryosphere–groundwater–river interactions; systematic mapping and protection of spring recharge zones; and risk-informed, multi-scale water planning that combines conjunctive use, decentralized storage, and community-based adaptation in the fragile Trans-Himalayan landscapes.
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