Sheikh Sameer
Kashmir has always lived with nature. Its seasons shaped its agriculture, its rivers sustained its settlements, its snowfall fed springs and streams, and its mountains provided a natural shield against the extremes of the subcontinent. For generations, people understood the rhythm of the Valley almost instinctively: winter meant snow, spring brought rain and blossoms, summer brought warmth, and autumn arrived with harvests.
That rhythm is changing.
Today, Kashmir’s environmental crisis is no longer something visible only in scientific reports or discussed at international climate conferences. It is increasingly being experienced in ordinary life—in warmer nights, disappearing snow, sudden downpours, flash floods, drying water sources, changing agricultural cycles, crop diseases, pest attacks and retreating glaciers.
And now comes another warning from the mountains.
A new study published in the Journal of Glaciology has classified five glacial lakes in the Kashmir Himalaya as having “very high” susceptibility to Glacial Lake Outburst Floods (GLOFs). Modelling indicates that a potential outburst could threaten 2,704 downstream buildings and 15 major bridges, besides roads and a hydropower project. The study assessed 155 glacial lakes using multiple indicators associated with GLOF susceptibility.
The five lakes—Bramsar, Chirsar, Nundkol, Gangabal and Bhagsar—are not simply remote geographical features. They are part of a mountain system whose water eventually connects with the valleys and communities below.
This should not be treated merely as another disaster-management statistic.
It should be treated as a warning about Kashmir’s changing relationship with nature.
The danger is no longer coming from one direction
Climate change rarely announces itself through one dramatic event. Its most dangerous characteristic is that it changes many things simultaneously.
A warmer atmosphere changes precipitation. Changing precipitation affects snowfall. Reduced snow affects glaciers and water storage. Glacier melt changes the behaviour of mountain lakes and rivers. Warmer conditions influence insects and pathogens. Altered rainfall affects crops. Extreme rainfall overwhelms drainage systems. Dry periods increase pressure on groundwater and springs.
One change feeds another.
This is why Kashmir’s climate story cannot be reduced to whether one particular winter received more or less snow than the previous year.
The real question is whether the entire climatic system on which Kashmir’s ecology and economy depend is becoming unstable.
Evidence from the Kashmir region points in that direction. A recent assessment reported several consecutive winters of below-normal precipitation, with reduced snowfall affecting natural water storage, rivers, irrigation, orchards and farms. Warmer winters have also been associated with changing agricultural conditions and increased pest outbreaks.
For a region historically dependent on winter snow, this is particularly significant.
When winter stops behaving like winter
Snow is not simply a beautiful covering over Kashmir’s mountains.
It is a natural reservoir.
Snow accumulated during winter is gradually released as temperatures rise. It feeds streams, springs, rivers and agricultural systems. It also contributes to the health of glaciers and mountain ecosystems.
When precipitation that would historically have fallen as snow instead arrives as rain, Kashmir loses part of this natural storage system.
Rain runs away quickly.
Snow stays.
That difference is fundamental.
A reduction in snowfall can therefore create a paradox: a region may experience intense rainfall and still face water shortages later in the year.
This is one of the reasons Kashmir’s changing precipitation pattern deserves far greater attention than simply comparing annual rainfall totals.
The timing of precipitation matters as much as its quantity.
If Kashmir receives less snow in winter but more intense rain during warmer months, the Valley can simultaneously face flooding and water scarcity.
That is the new climate contradiction.
The warming of both days and nights
Perhaps one of the most important indicators of climate change is not merely the occurrence of extremely hot days but the gradual warming of nights.
The Hindu Kush Himalayan region has experienced rising temperatures, with research showing increases in warm days and warm nights and declines in cold days and nights over recent decades.
For Kashmir, warmer nights have consequences extending far beyond human discomfort.
Plants respond to temperature.
Insects respond to temperature.
Soil responds to temperature.
Snow responds to temperature.
Glaciers respond to temperature.
Even the timing of flowering and pollination responds to temperature.
A warmer night means that the landscape receives less of the cooling that historically formed part of Kashmir’s seasonal cycle.
This can disturb plant development, increase evaporation and influence agricultural pests and diseases.
The danger, therefore, is not simply that Kashmir may become hotter.
It is that Kashmir’s ecological clock may gradually lose its traditional rhythm.
Rain that arrives at the wrong time
For farmers, rainfall is useful only when it arrives at the right time and in the right quantity.
A prolonged dry period followed by an intense downpour is not equivalent to steady precipitation distributed across the season.
Sudden heavy rainfall can wash away soil, damage standing crops, trigger landslides and overwhelm drainage systems.
Kashmir’s mountainous geography makes the situation more complicated. Steep slopes accelerate runoff, while narrow valleys concentrate water.
The result can be devastating.
A cloudburst or intense rainfall event in the upper catchments can transform a relatively peaceful stream into a destructive torrent within a short period.
And as climate change alters precipitation patterns, the distinction between an ordinary rainy season and an extreme rainfall event becomes increasingly important.
The glaciers: Kashmir’s silent warning system
Glaciers are among the clearest indicators of long-term climatic change.
They respond slowly to climate variations, but once sustained warming sets in, their retreat can become a profound ecological and hydrological problem.
Kashmir’s glaciers are not merely frozen landscapes for tourists and mountaineers. They are part of the region’s water infrastructure.
Their meltwater contributes to rivers and streams and helps sustain ecosystems downstream.
But glacier retreat creates a dangerous transition.
Initially, accelerated melting can increase water availability.
Later, as glacier mass declines, that contribution can weaken.
At the same time, melting ice and destabilised mountain terrain can contribute to the formation or expansion of glacial lakes.
This is where the latest study becomes particularly important.
Five Kashmir glacial lakes have now been classified in the very-high GLOF susceptibility category. A potential outburst could affect thousands of structures and critical infrastructure downstream.
The danger is not that these lakes will necessarily burst tomorrow.
The danger is that the risk exists—and that a combination of warming, unstable slopes, earthquakes, avalanches or other triggering events could turn a high-altitude lake into a rapidly moving wall of water and debris.
The Nepal warning
Events elsewhere in the Himalayas should make Kashmir sit up and take notice.
The catastrophic flooding recently witnessed in Nepal has again demonstrated how quickly mountain systems can become dangerous. Scientists and climate experts have warned that warming, glacier instability, melting ice and changing mountain conditions are increasing hazards across the Himalayan region.
Kashmir should not assume that geography will protect it.
The Himalayas are interconnected through climate and geology even when administrative boundaries divide them.
A disaster in Nepal is therefore not simply a Nepali problem.
It is a warning for every Himalayan community.
Indeed, Jammu and Kashmir authorities are already working on early-warning systems at several hydropower projects, including Baglihar, Upper Sindh and Parnai, while also developing broader multi-hazard risk planning.
The fact that such preparations are becoming necessary tells us something important: the definition of disaster risk in Kashmir is changing.
Agriculture is becoming an early casualty
Perhaps nowhere is climate change more intimately felt than in Kashmir’s orchards and agricultural fields.
Apple, cherry, walnut, paddy, vegetables and other crops depend upon carefully balanced temperature and precipitation patterns.
When temperatures change, flowering can occur earlier.
When flowering occurs earlier, an untimely frost can cause greater damage.
When humidity and temperature change, fungal infections and other crop diseases may become more favourable.
When winters become warmer, certain pests may survive conditions that previously suppressed them.
When rainfall becomes erratic, farmers can face drought and waterlogging within the same growing season.
Climate change therefore does not have to destroy a crop directly.
It can gradually make farming more unpredictable.
And unpredictability is itself an economic burden.
A farmer can adapt to a known risk.
It is much harder to adapt when the old calendar no longer reliably tells him when to sow, irrigate, spray, prune or harvest.
Research on Kashmir’s agricultural communities has documented warming trends across seasons and growing concerns about the effects of climate change on irrigated agriculture and horticulture.
Diseases are another invisible threat
Climate change is also changing the biological environment.
Plants, insects, fungi and pathogens all respond to temperature and moisture.
A warmer environment can alter the geographical range and seasonal behaviour of pests. Changes in rainfall and humidity can influence plant disease development.
This creates a chain reaction:
climate change → altered temperature and moisture → altered pest and pathogen behaviour → crop damage → economic loss.
It is an invisible form of environmental change.
There may be no dramatic flood photograph.
No collapsing mountain.
No roaring river.
Yet a farmer may discover that an orchard which was once relatively manageable now requires greater expenditure on disease control and pest management.
The cost of climate change can therefore appear quietly in household budgets.
Floods and the paradox of water
Kashmir’s future water problem may be particularly complicated.
On one side there is the possibility of more intense rainfall and sudden flooding.
On the other is declining snowpack and changing glacier behaviour.
These are not contradictory.
They can happen together.
Imagine a mountain catchment receiving less winter snow but experiencing an intense summer rainfall event. The snowpack is weaker, but the rainfall produces rapid runoff. Rivers rise quickly, while there is less stored snow available to sustain water flows later.
Thus Kashmir can move from
That is why flood management and water-security planning cannot be separated anymore.
Nature is also warning us about our own development
Climate change is only one part of the problem.
Human activity can turn a climate hazard into a disaster.
Construction along floodplains, encroachment of wetlands, destruction of natural drainage channels, unplanned urban expansion, deforestation, hill cutting and poorly planned infrastructure can all increase vulnerability.
A heavy rainfall event is a natural phenomenon.
But whether it becomes a catastrophe depends partly on what human beings have built in its path.
The Himalayas are geologically young and fragile. Experts increasingly emphasise that uncontrolled development in vulnerable mountain areas can amplify climate-related hazards. �
The Times of India
Kashmir therefore needs to stop asking only:
“How severe was the rainfall?”
It must also ask:
“Why did the rainfall cause so much damage?”
Are we becoming the first victims?
Calling Kashmir the “first victim of climate change” needs some qualification.
Kashmir is certainly not literally the world’s first climate-change victim. Communities across the globe, from small island states to Arctic populations and drought-stricken regions, are already experiencing severe consequences.
But Kashmir can legitimately be described as an early and highly vulnerable victim of Himalayan climate change.
Its vulnerability comes from geography, dependence on natural water systems, agriculture, horticulture, tourism and fragile mountain ecosystems.
Kashmir sits at the intersection of several climate-sensitive systems.
Its mountains are warming.
Its glaciers are changing.
Its snow patterns are shifting.
Its rainfall is becoming less predictable.
Its agriculture is vulnerable.
Its rivers can turn destructive.
Its population and infrastructure are expanding.
And its natural buffers—wetlands, forests, floodplains and open drainage systems—are under pressure.
This combination makes Kashmir particularly exposed.
The unseen danger is complacency
Perhaps the greatest danger is not the glacier lake itself.
It is complacency.
A GLOF warning is dramatic because it has a name and a number: five lakes, 2,704 buildings, 15 bridges.
But climate change is much bigger than those figures.
The real warning is visible in hundreds of smaller changes:
A winter without snow.
An unusually warm January day.
A spring arriving early.
An orchard flowering at the wrong time.
A sudden cloudburst.
A stream drying earlier than expected.
An unfamiliar pest appearing in a crop.
A mountain slope becoming unstable.
A flood where residents thought flooding was unlikely.
None of these events alone proves climate change.
Together, however, they form a pattern that Kashmir can no longer afford to ignore.
Kashmir needs a climate-security strategy
The response cannot simply be planting a few trees or issuing occasional weather advisories.
Kashmir needs a comprehensive climate-resilience strategy.
First, every high-risk glacial lake needs systematic monitoring, including satellite surveillance, field assessment and early-warning systems.
Second, downstream communities need evacuation plans. A warning is useless if people do not know where to go.
Third, floodplains and natural drainage channels must be protected from reckless construction.
Fourth, wetlands must be treated as natural flood-control infrastructure, rather than vacant land waiting for development.
Fifth, Kashmir needs better snow, glacier and groundwater monitoring so that future water availability can be predicted.
Sixth, farmers require climate-resilient agricultural practices, disease surveillance, improved irrigation and timely weather information.
Seventh, urban planning must acknowledge that extreme rainfall events are becoming a serious risk.
And finally, climate science needs to move from research institutions into public policy.
The choice before Kashmir
Kashmir cannot control the global climate by itself.
Its contribution to global greenhouse-gas emissions is tiny compared with that of major industrial economies.
But Kashmir can control how vulnerable it chooses to remain.
The question is no longer whether climate change exists.
The question is whether we will continue planning Kashmir as if the climate of the twentieth century is guaranteed to continue through the twenty-first.
It isn’t.
The mountains are telling us.
The glaciers are telling us.
The snowfall is telling us.
The farmers are telling us.
The rivers are telling us.
And now, the classification of five glacial lakes is telling us in scientific language what nature has been signalling for years.
Kashmir is not simply losing snow. It is losing climatic predictability.
That may ultimately prove more dangerous than rising temperatures themselves.
Because a society can prepare for heat.
It can prepare for rain.
It can prepare for snow.
But preparing for a climate whose behaviour is becoming increasingly uncertain is much harder.
The unseen danger from nature is therefore not one catastrophic event waiting somewhere in the mountains.
It is the slow transformation of the environmental system upon which Kashmir’s life has depended for centuries.
The choice before us is stark: adapt before nature forces us to adapt.
For Kashmir, climate change is no longer a distant threat.
It is already knocking on the door.
And the latest warning from the glaciers suggests that the mountains may be knocking the loudest.





