Srinagar, Oct 17: Kashmir’s water crisis may be unfolding long before its rivers run low. High in the Himalayas, where winter snowfall stores water for the warmer months, a worrying shift in snow cover and repeated winter precipitation deficits are raising fresh questions about the Valley’s long-term water security.
A satellite-based study published in the journal Climate in 2025 found that the snow-covered area across Jammu and Kashmir declined from 22,261.21 square kilometres in 2000 to 15,275.75 square kilometres in 2024 — a reduction of around 31.4 per cent. The findings underline the importance of monitoring the region’s changing snow cover and its implications for seasonal water availability.
The warning comes against the backdrop of seven consecutive winters with below-normal precipitation in Jammu and Kashmir. Independent weather forecaster Faizan Arif’s data showed that the core winter period from December 2025 to February 2026 ended with a 65 percent precipitation deficit, with the region receiving 100.6 mm against a normal of 284.9 mm.
“February was particularly dry, recording just 14.2 mm of precipitation against the normal of 130.4 mm — a deficit of nearly 89 per cent. Kishtwar recorded a 90 per cent deficit, followed by Shopian at 82 per cent, while Srinagar and Jammu recorded deficits of 64 per cent each,” the data notes.
The figures point to a growing challenge for a region whose rivers, springs, wetlands, agriculture and drinking-water supplies depend heavily on the seasonal rhythm of rain and snow.
Climate expert Dr Touseef Ahmad Bhat said the changing climate must be viewed alongside the degradation of Kashmir’s natural ecosystems, which play a critical role in regulating water flows and protecting communities from environmental extremes.
“When forests are degraded, wetlands disappear, and mountains are disturbed through unplanned construction, even moderate rainfall can trigger disasters. Climate change and ecological degradation together create a dangerous combination,” Bhat has warned.
His concerns highlight a crucial dimension of Kashmir’s emerging water challenge: the region is not only confronting shifts in precipitation but also losing natural systems that help absorb, store and gradually release water. Snowfall in the higher reaches acts as a natural reservoir, with melting snow feeding streams and rivers during spring and summer. When snow cover becomes less persistent or melts earlier, the timing of water availability can change, putting pressure on irrigation, horticulture and drinking-water supplies when demand rises.
Arif has cautioned that repeated winter deficits are weakening this natural buffer.
“With December almost dry, January subpar and February collapsing nearly 90 per cent below normal, the snowpack generation window has weakened substantially,” Arif said.
He has also highlighted changes in the distribution of precipitation, including longer dry spells between active weather systems. Such fluctuations matter because seasonal totals alone do not reveal whether water is arriving at the right time or being stored in the mountains for use during warmer months. Sonam Lotus, Director of the Meteorological Centre in Ladakh, has emphasised the need to assess long-term records before drawing conclusions about changing snowfall patterns.
“Analysis of the past 43 years of data shows that there have been years when snowfall has been lower than what has been received this winter,” Lotus said, cautioning against early conclusions.
A study published in the journal MAUSAM in January 2026, examining precipitation trends across Jammu and Kashmir between 1980 and 2020, also identified significant declining trends in annual precipitation at the stations studied. It reported declining trends during parts of the pre-monsoon and post-monsoon seasons, although the scale of change varied across locations and months.
Together, the findings point to the need for a more comprehensive understanding of how snowfall, rainfall, rising temperatures and land-use changes interact to affect water availability.
For Kashmir, the consequences extend well beyond the rivers. Reduced or less predictable snowmelt can affect orchards, paddy cultivation, groundwater recharge and springs, while prolonged dry periods can increase pressure on drinking-water systems. Sudden heavy rainfall, meanwhile, can create flooding and erosion risks, particularly where wetlands, forests and natural drainage channels have been degraded. The challenge is therefore not simply whether Kashmir receives less precipitation in a particular year. It is whether the region can retain enough water in its natural reservoirs and ecosystems to meet demand throughout the year. Experts say a coordinated monitoring system linking snowfall records, satellite-based snow-cover assessments, glacier observations, spring discharge and river-flow measurements would help policymakers anticipate shortages rather than respond after they emerge.
The evidence does not suggest that Kashmir’s rivers are about to run dry. It does, however, raise a serious question about the reliability of the natural water cycle on which millions of people and livelihoods depend. As the Himalayas continue to store and release water under changing climatic conditions, protecting Kashmir’s forests, wetlands, springs and mountain catchments may prove as important as measuring how much rain and snow the region receives.
