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Beyond the Ban: Understanding Fire Season in the Western Ghats

  • Writer: Nagabhushan M N
    Nagabhushan M N
  • 2 days ago
  • 7 min read

You've seen the notices. The permit denials. The Facebook posts from frustrated trekkers asking, "Why can't we just hike responsibly?"

Here's the truth: This isn't about bureaucracy. This is about physics, ecology, and the very real possibility that one wrong spark could erase ecosystems that took millennia to build.

The 2026 trekking ban across Karnataka's Western Ghats isn't a restriction—it's a recognition. A recognition that we're standing at the edge of a climate threshold where the mountains we love could become the mountains we mourn.

This post isn't about finding loopholes. It's about understanding why the fire season has turned the Western Ghats into a landscape where adventure and disaster sit closer together than ever before.



The Global "Water Tower" at Risk

The Western Ghats aren't just a trekking destination. They're a 1,600-kilometer lifeline.

Designated as a UNESCO World Heritage site, this ancient mountain range functions as India's primary "water tower"—capturing monsoon rains, filtering them through dense shola grasslands and forests, and releasing them gradually through rivers that feed 245 million people. The Godavari. The Krishna. The Kaveri. These aren't just rivers; they're the reason South India has drinking water in April.

But here's what most trekkers don't see: The entire range—from the Bhimashankar forests in Maharashtra down to the Agasthyamalai peaks in Kerala—operates as a single, interconnected system. When one section burns, the smoke doesn't respect state borders. The ecological damage doesn't stop at a district line.

The trekking ban in Karnataka is part of a larger, systemic response to a landscape under stress. During the fire season (January through May), these mountains transform from water storage systems into fuel repositories. The very grasses that make summit ridges so photogenic turn into golden accelerants waiting for ignition.

This isn't about restricting your freedom. It's about protecting a landscape that holds the future of Southern India's water security.

Case Studies: When the Mountains Burnt




Let's talk about what happens when prevention fails.

2018: The Kurangani Tragedy (Tamil Nadu)

March 11, 2018. Eighteen trekkers set out for a routine expedition in the Theni district's grasslands. They never came back.

A Western Ghats forest fire erupted with terrifying speed. The dry season had turned the slopes into tinder. High-altitude winds pushed flames across the landscape faster than a human can sprint. The trekkers found themselves trapped in a narrow valley with no escape routes, no water sources, and smoke so thick it choked out visibility within minutes.

The aftermath changed policy across South India. It proved—tragically—that during peak fire season, the Ghats offer zero margin for error. The wind-swept grasslands provide no shelter. The steep terrain eliminates escape. And once the fire begins, you have minutes, not hours.

2019: The Bandipur Mega-Fire (Karnataka/Tamil Nadu)

Over 10,000 acres. That's the scale of destruction when a Western Ghats forest fire crosses the threshold from incident to catastrophe.

The Bandipur fire started small. But in the drought conditions of late February, it exploded across state borders into Mudumalai. Satellite imagery captured smoke plumes so massive they were visible from space. Air quality deteriorated as far as Kerala, hundreds of kilometers away.

Forest departments from three states coordinated response efforts. Despite deploying hundreds of personnel, the fire burned for days. The damage? Irreversible loss to wildlife corridors, watershed degradation, and the destruction of old-growth forests that won't recover in our lifetimes.

2024-2025: The Maharashtra Konkan Belt

More recently, the northern Sahyadris experienced something new: unseasonal flash fires in areas like Ratnagiri and Raigad.

The culprit? A combination of heatwaves, invasive grass species, and earlier-than-expected dry conditions. Local authorities, unprepared for fires outside the traditional season, struggled to contain blazes that moved with unprecedented speed.

The pattern is clear: The fire season is extending. The intensity is increasing. The predictability we once relied on no longer exists.

The Anatomy of a Shola-Grassland Disaster

To understand why these fires are so catastrophic, you need to understand the architecture of high-altitude Western Ghats ecosystems.

The Sky Islands

Peaks like Kudremukh, Anamudi, and Kalsubai function as "sky islands"—isolated pockets of unique biodiversity separated by valleys and plateaus. These aren't just scenic viewpoints. They're evolutionary laboratories where species exist nowhere else on Earth.

The shola grasslands at these elevations operate as a mosaic: patches of dense, moisture-retaining shola forests interspersed with rolling grasslands. This pattern isn't random. It's the product of thousands of years of monsoon cycles, soil composition, and microclimatic conditions.

The Fire Trap: A Three-Part System

The Grass (The Fuel)

During January through May, the grasses dry out completely. What was green and supple in October becomes brittle, golden fuel with moisture content below 10%. One square kilometer of this grassland contains enough combustible material to sustain a fire for hours.

The Wind (The Accelerator)

High-altitude winds in the Ghats average 30-40 km/h during dry season. But in narrow valleys and ridge systems, they can gust to 60+ km/h. These winds don't just spread fire—they preheat vegetation ahead of the flames, creating conditions where ignition happens before the fire front even arrives.

A spark in these conditions can become a wall of flame moving at 15-20 km/h. That's faster than you can descend a steep trail with a backpack.

The Shola (The Victim)

The shola forest patches are the real tragedy. These dense, moisture-laden forests act as ecological sponges—absorbing rainfall and releasing it gradually through underground springs. They're the reason streams flow in April when the last monsoon was six months ago.

Once fire enters a shola, the damage is catastrophic. The upper canopy chars. The understory—which takes 50-100 years to establish—burns completely. The soil, stripped of its protective layer, erodes during the next monsoon. And the springs? They dry up, sometimes permanently.

The "Human Factor" (90% of All Fires)

Here's the uncomfortable truth: Nature doesn't start these fires. We do.

Forest department data shows that over 90% of Western Ghats forest fires have human origins. Let's break down how it happens.

The Negligence

A cigarette butt tossed from a moving vehicle. A campfire inadequately extinguished. A cooking stove left unattended while trekkers explore a nearby viewpoint.

These aren't hypothetical scenarios. They're the documented causes of actual fires. A single ember in 12% humidity grassland is all it takes.

The Sabotage

This is harder to discuss, but it's real. Some fires are set intentionally—by poachers clearing sightlines, by locals encouraging fresh grass growth for cattle, or by land grabbers attempting to clear forest land for development.

The problem? What might be a "controlled" burn in a normal year becomes an uncontrollable inferno during a drought. The person who set the fire is long gone by the time it reaches crisis scale.

Invasive Species: The Wooden Petrol

Lantana camara. Remember this name.

This invasive weed is taking over degraded forest areas across the Western Ghats. And here's what makes it particularly dangerous: Lantana burns three times hotter than native vegetation.

When a fire moves through lantana-infested areas, it generates enough heat to kill trees that would normally survive. It creates fire intensities that native species have no evolutionary defense against. And after the fire? Lantana is among the first to regrow, crowding out native seedlings and setting the stage for even worse fires in the next cycle.

It's a positive feedback loop that's transforming fire-resistant ecosystems into fire-prone wastelands.

"A single unextinguished campfire in lantana-infested grassland can reach temperatures of 800°C—hot enough to sterilize soil and kill seed banks buried 10cm underground."

Why the 2026 Ban is Different

Every year sees fire risk. But 2026 isn't every year.

The El Niño Effect

The 2025-2026 cycle brought a significant rainfall deficit across the Western Ghats. October through December saw 30-40% below-normal precipitation in critical areas. This isn't just about surface dryness—soil moisture levels at depth are at multi-decade lows.

What does this mean practically? The underground water reserves that normally keep shola forests moist are depleted. The vegetation is stressed. The fuel load is higher and drier than climatological averages.

We're not dealing with typical fire season conditions. We're dealing with worst-case scenario conditions.

The "Chimney Effect"

Here's the physics that makes narrow valleys lethal: Fire creates its own weather.

As flames consume oxygen and release heat, they generate powerful updrafts. In confined valleys and gorges, these updrafts create what's known as a "chimney effect"—pulling in air from surrounding areas and feeding the fire with fresh oxygen while simultaneously creating vacuum conditions nearby.

What this means for trekkers: You can be a kilometer away from visible flames and still die from oxygen depletion or heat exhaustion. The rising superheated air can create ground-level temperatures of 60°C in shaded areas. Your lungs can't handle breathing air that hot. Your body can't cool itself when ambient temperature exceeds skin temperature.

This isn't about being "careful with fire." This is about being in the wrong place when atmospheric conditions turn a hillside into a convection oven.


The Wanderophile Pledge: Timing is Everything

Real adventure isn't about forcing your way onto a mountain during fire season. It's about understanding that timing separates memorable experiences from preventable tragedies.

If we push into the Western Ghats during the trekking ban period, we're not just risking our lives. We're risking the complete loss of ecosystems that have survived for thousands of years. We could be the generation that saw the sholas disappear—not because of climate change abstractions, but because we couldn't wait four months.

The mountains will be there in June. The question is: Will they still be forests, or will they be ash?

What You Can Do Right Now

Support the Forest Department. They're not the enemy. They're the understaffed, underfunded teams trying to protect something irreplaceable. If you see policy criticism online, counter it with science, not frustration.

Report illegal treks. If you spot groups advertising Western Ghats treks during the ban period, report them. These aren't "rebels"—they're saboteurs putting everyone at risk.

Shift your gaze. Karnataka offers extraordinary landscapes that are safe, accessible, and spectacular during the dry season. Hampi's boulder fields. Gokarna's coastal trails. Dandeli's river gorges. These aren't consolation prizes—they're world-class destinations in their own right.

The Bigger Picture

This ban is temporary. The damage from a catastrophic fire isn't.

The Western Ghats have survived ice ages, tectonic shifts, and climate fluctuations. They've given us water, biodiversity, and landscapes that define what we think of as "Southern India."

But they can't survive us if we refuse to listen.

Real explorers adapt. They read the conditions. They respect the rhythm of the landscape. And they understand that sometimes, the most adventurous thing you can do is wait.

Ready to explore safely? Check out where we're actually heading this season —Hampi's sunrise climbs, Gokarna's coastal trails, and Dandeli's whitewater adventures. All timed for when Karnataka's wilderness is open and ready.

The mountains aren't going anywhere. Let's make sure they stay green.

 
 
 

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