menu_open Columnists
We use cookies to provide some features and experiences in QOSHE

More information  .  Close

Kashmir’s changing water reality

38 0
22.05.2026

For centuries, water has been the soul of Kashmir. From the sacred springs (Naag) beneath majestic Chinar trees to the snow-fed rivers descending from the Himalayas, water has shaped the Valley’s culture, traditions, economy, and everyday life. Villages grew around springs, wetlands sustained biodiversity and agriculture, and snowfall in the mountains quietly nourished life in the plains below. Yet today, this delicate natural balance is facing unprecedented stress. 

Kashmir is witnessing a silent yet deeply concerning transformation in its water systems. Over the past few decades, Kashmir has witnessed noticeable climatic changes marked by declining snowfall, rainfall deficits, rising summer temperatures, and changing precipitation patterns. Glaciers across the Valley are retreating, snow persistence is reducing, and both surface and groundwater systems are showing signs of stress. Streams that once carried strong discharge during summer are now witnessing reduced flow. Springs that remained perennial for generations are showing declining discharge, while some are drying earlier than usual. Wetlands are shrinking, catchment areas are degrading, and groundwater recharge is steadily declining.

The Changing Hydrology of KashmirSnow has always functioned as Kashmir’s natural water bank. Unlike rainfall, snow stores water during winter and releases it gradually during spring and summer, thereby sustaining rivers, springs, wetlands, agriculture, and groundwater recharge systems during the lean season. However, reduced snow persistence and rising temperatures are altering the Valley’s natural hydrological cycle. Earlier snowmelt is changing the timing and availability of water resources across the region. As a result, rivers such as the Jhelum River increasingly experience comparatively higher flows during spring, followed by reduced discharge during peak summer months - precisely when demand for drinking water, irrigation, horticulture, and domestic use reaches its highest level. Even during years receiving near-normal snowfall, early melting lowers........

© Greater Kashmir