Erratic winter precipitation in the Western Himalayas is an emerging climate risk. Discuss with reference to snow drought, glacier health and mountain tourism.

Most winter snow in the Western Himalayan Region (WHR) comes from Western Disturbances (WDs). These are extratropical low-pressure systems, and IMD tracks them spell by spell [2]. When WDs come late, come weak or come in sudden bursts, the effects add up. Water, ice and the mountain economy all lose together, so erratic winter snow is a real and growing climate risk.

Snow drought: the water risk

• Missed or delayed WDs leave a thin snowpack. Springs then recharge less, and less snowmelt reaches Kashmir's orchards and Rabi crops in summer.
• Burst-type spells are replacing steady snowfall. IMD tracked one intense WD as a single spell from 22 to 26 January 2026, with heavy falls over the Kashmir valley on 22–23 January [2]. Short, heavy spells like this cannot always make up for a dry early winter.

Glacier health: the long-term risk

• Winter snow is how glaciers gain mass. Several poor snow years in a row shrink glaciers and expose darker ice, which melts faster.
• This threatens the lean-season flow of Indus-basin rivers such as the Jhelum and Chenab. It also hits hydropower and drinking-water supply.

Mountain tourism: the economic and safety risk

• Livelihoods: Gulmarg's winter economy depends on snow. Fresh snow at Kangdoori on 11 November 2026 drew crowds at the "peak of the season" [1]. Winters with little snow mean cancelled bookings and lost income.
• Hazard: The same fresh snow loads slopes and raises avalanche risk. DGRE runs 72 snow-meteorological observatories, but only 45 automatic weather stations are working; the rest are still being tested or installed [3].
• Warning gap: Bulletins were built mainly for the Army [4]. NDMA's avalanche guidelines date from 2009 [5], before CAP-based alerts existed [3].

Way forward

• Finish the planned AWS network and extend avalanche radar from North Sikkim to busy tourist slopes [3].
• Name tour operators and ski-slope managers as receivers of CAP alerts, and update the 2009 NDMA guidelines [5].
• Publish a season-end figure for the WHR showing snowfall against normal, so that planning rests on data and not on single events [2].
• Diversify into all-season tourism and expand glacier mass-balance monitoring.

Snow drought, glacier loss and tourism risk all come from the same cause: unpredictable WDs. Better forecasting, early warnings that reach the public, and adaptive livelihoods can turn this risk into resilience. This fits the Sendai Framework and SDG 13 on climate action.