What Happened
- The Jhelum River at Sangam in south Kashmir dropped to minus 0.86 feet on March 5, 2026 — below the zero-gauge mark during a period when snowmelt typically raises water levels.
- Jammu and Kashmir recorded its seventh consecutive rainfall-deficient winter; precipitation between December and February was only 100.6 mm against a normal of 284.9 mm — a deficit of nearly 65%.
- Srinagar recorded 24.7°C (approximately 11.7°C above normal) and Gulmarg reached 17.2°C (13.7°C above normal), with Gulmarg experiencing its highest temperature ever recorded in March.
- February was especially severe: Srinagar received just 5.3 mm of rainfall.
- Changing precipitation patterns — rain falling instead of snow — combined with accelerated evaporation and glacial retreat are driving the crisis.
Static Topic Bridges
Indus Waters Treaty (IWT) and the Jhelum
The Indus Waters Treaty was signed on September 19, 1960, between India and Pakistan with World Bank mediation, by Prime Minister Jawaharlal Nehru and Pakistani President Ayub Khan. Under the treaty, the three western rivers — Jhelum, Chenab, and Indus — were allocated primarily to Pakistan, while India received the three eastern rivers — Ravi, Beas, and Sutlej. Pakistan received roughly 80% of total water flows, while India retained 20%.
- The Jhelum is a "western river" under the IWT — Pakistan has unrestricted use with limited exceptions.
- India can use the Jhelum for non-consumptive purposes such as navigation, hydropower (run-of-river), and limited irrigation.
- The Tulbul Navigation Project on the Jhelum has been stalled since the 1980s due to Pakistan's objections that it could give India control over downstream flows.
- A Permanent Indus Commission meets annually to resolve disputes; extraordinary disputes go to a Neutral Expert or Court of Arbitration.
Connection to this news: A dramatic reduction in Jhelum flows due to climate change has direct implications for downstream water availability in Pakistan and could strain treaty obligations, potentially becoming a new flashpoint for India-Pakistan water diplomacy.
Glacial Retreat and Himalayan Hydrology
The Himalayas contain the largest concentration of glaciers outside the polar regions, often called the "Third Pole." These glaciers are critical to the water security of South Asia, feeding river systems including the Indus basin. Kashmir's glaciers lost 5.2 square kilometres between 1980 and 2013. Accelerated glacial retreat causes an initial surge in river flows (glacial lake outburst floods), followed by long-term water scarcity as glacier mass is depleted.
- India has over 9,500 glaciers covering approximately 37,000 sq km in the Himalayan region [Unverified exact figure].
- The Hindu Kush Himalaya Assessment (2019) by ICIMOD projected that glaciers in the region could lose one-third of their mass by 2100 even if emissions are controlled.
- Western Disturbances (extra-tropical cyclones originating in the Mediterranean/Atlantic) are the primary winter precipitation mechanism for J&K; weakening or shifting of these systems drives deficits.
- The phenomenon of "rain-on-snow" — rain falling on frozen snowpack — accelerates runoff and reduces long-term water storage.
Connection to this news: Seven consecutive deficit winters and above-normal temperatures point to a structural weakening of Western Disturbances and accelerated glacial mass loss in the Kashmir Himalaya, threatening the long-term viability of the Jhelum as a perennial river.
Agriculture and Water Security in a Changing Climate
Kashmir's paddy cultivation is critically dependent on Jhelum water availability. India's National Water Policy (2012) prioritises drinking water and then agriculture in water allocation. The National Action Plan on Climate Change (NAPCC, 2008) includes the National Mission for Sustaining the Himalayan Ecosystem as one of its eight missions, specifically addressing glacial retreat.
- NAPCC was launched in 2008 under PM Manmohan Singh; the National Mission for Sustaining the Himalayan Ecosystem focuses on monitoring glaciers, biodiversity, and river flows.
- The National Water Policy (2012) calls for integrated basin-level water management and demand-side efficiency measures.
- Drip irrigation and micro-irrigation are supported under the Pradhan Mantri Krishi Sinchayee Yojana (PMKSY), aimed at "more crop per drop."
- Experts recommend a crop shift from water-intensive paddy to dryland crops like maize, pulses, and oilseeds to adapt to water scarcity in Kashmir.
Connection to this news: The historic low in the Jhelum directly threatens the kharif paddy sowing season in Kashmir, making adaptation strategies — crop diversification, micro-irrigation, and water harvesting — urgent policy priorities aligned with NAPCC and PMKSY.
Western Disturbances and India's Winter Climate
Western Disturbances (WDs) are extra-tropical cyclonic storms that originate in the Mediterranean Sea, Caspian Sea, or Black Sea and travel eastward across West Asia and Afghanistan before bringing winter precipitation to northwestern India, including J&K. They are the primary source of winter snowfall in the Himalayas and pre-monsoon rainfall in the Indo-Gangetic Plain.
- WDs typically affect India between November and March, bringing snowfall above 2,000 metres and rainfall in the plains.
- Climate models suggest WDs are becoming less frequent but more intense as global warming progresses.
- The India Meteorological Department (IMD) issues Western Disturbance advisories as they are associated with fog, cold waves, and flash floods in the mountains.
- The 65% precipitation deficit in J&K for Dec 2025–Feb 2026 is consistent with a weakened or poorly tracked WD season.
Connection to this news: The absence of adequate Western Disturbances this winter is the proximate cause of Kashmir's precipitation deficit and the consequent record-low Jhelum levels.
Key Facts & Data
- Jhelum River at Sangam: minus 0.86 feet on March 5, 2026 (historic low for the season)
- J&K precipitation deficit (Dec 2025–Feb 2026): ~65% (100.6 mm vs. normal 284.9 mm)
- Srinagar max temp: 24.7°C (11.7°C above normal); Gulmarg: 17.2°C (13.7°C above normal)
- Kashmir glacial loss: 5.2 sq km between 1980 and 2013
- Indus Waters Treaty signed: September 19, 1960; World Bank facilitated
- Jhelum is classified as a "western river" under IWT — allocated primarily to Pakistan
- Seven consecutive deficit winters recorded in J&K