By Dipak Kurmi
For centuries, Cherrapunji—locally known as Sohra—has carried an aura of mystique, celebrated as one of the wettest places on Earth. Alongside its twin, Mawsynram, perched on the southern escarpment of the Khasi Hills in Meghalaya, this town has been immortalized in school textbooks, travelogues, and meteorological records for its relentless downpours. The sheer excess of rain, measured not in hundreds but in thousands of millimeters, had made Cherrapunji a living symbol of abundance in water, where clouds seemed never to pause in their gift-giving. Yet, the monsoon of 2025 has revealed a disconcerting truth: even the wettest place on Earth can fall silent beneath the weight of deficit skies.
Between June 1 and August 20 of this year, Sohra’s weather station, maintained by the India Meteorological Department (IMD), logged around 3,500 millimeters of rainfall—staggeringly below its seasonal norm. This is nearly 50 percent less than expected, a figure that jars with the historical legacy of uninterrupted torrents. To put this in context, Cherrapunji’s average monsoon rainfall stands at approximately 8,131.9 millimeters, a figure once deemed untouchable. The lowest ever recorded monsoon rainfall at Sohra, dating back to 1962, was 5,401 millimeters. Unless some 1,900 millimeters of rain fall in the remaining stretch of the season between August 20 and September 30, this year will mark the leanest monsoon in its recorded history.
What makes this development more striking is the comparative rainfall landscape across India. While Cherrapunji, synonymous with excess, languished at half its quota, places far removed from Meghalaya stole the spotlight. In Karnataka’s Kodagu district, the Surlabbi station received nearly 7,300 millimeters of rainfall by August 18, of which 5,951 millimeters came during the monsoon alone. This is not only double the rainfall of Sohra during the same period but also the highest in India so far this year. In Maharashtra, Tamhini recorded 5,788 millimeters of rainfall just between June and July, while Surlabbi posted 4,931 millimeters in the same two months. By comparison, Cherrapunji could only manage 2,047 millimeters in June and July combined.
According to independent weather analyst R. Pardeep John, widely known as the Tamil Nadu Weatherman, at least 32 rainfall stations across India received more rain than Cherrapunji during the first two months of the monsoon in 2025. The reversal of expectations, where India’s famed “rain capital” finds itself outpaced by regions like the Western Ghats, is an indication of the shifting dynamics of the monsoon system.
The broader picture within Meghalaya paints an even more sobering narrative. The state as a whole is experiencing a 43 percent rainfall deficit this monsoon season, the highest deficit across all states in India. Of its eleven districts, six are classified as deficient, receiving 20 to 59 percent less rain than normal, while two fall under the “large deficient” category, with deficits ranging from 60 to 99 percent. West Jaintia Hills has borne the brunt, recording a staggering 75 percent deficit as of August 26. Even East Khasi Hills, home to both Sohra and Mawsynram, has recorded 29 percent less rainfall than usual.
This drying trend is not an isolated anomaly but part of a larger climatic shift that has been unfolding over the past decades. Climate scientists have been observing a decline in rainfall levels in Northeast India, a region once synonymous with lush greenery, flowing rivers, and an overabundance of water. Cherrapunji and Mawsynram, despite their record-setting past, are now struggling to maintain their legendary status. This year alone, both have registered nearly 50 percent below-normal rainfall.
To appreciate the magnitude of this change, one must understand why Cherrapunji and Mawsynram have historically been such rainfall magnets. Their unique geography is the central reason. Located on the southern slopes of the Khasi Hills, these towns directly face the Bay of Bengal branch of the southwest monsoon. As the moisture-laden winds travel northward, they collide with the steep escarpments of the Khasi Hills. With no path forward, the winds are forced to rise rapidly. This orographic effect leads to condensation and the release of torrential rains. The topography essentially traps the clouds, turning them into relentless rainmakers.
This natural phenomenon explains why Mawsynram holds the record for the highest annual rainfall in the world and why Cherrapunji has documented some of the heaviest rainfall events ever, including the astounding 2,493 millimeters recorded over just 48 hours in June 1995. For generations, these numbers underscored the inevitability of rain in Sohra, creating an almost mythological aura around the region. Tourists flocked not just to witness the stunning waterfalls and misty valleys but also to experience the rare phenomenon of near-constant rainfall.
Yet the monsoon of 2025 underscores the fact that even such seemingly eternal patterns are vulnerable to the vagaries of climate change and atmospheric shifts. The decline in rainfall in Northeast India has been attributed to multiple factors, ranging from deforestation and land-use changes to larger climatic trends linked to global warming. The Bay of Bengal monsoon currents are no longer as consistent in their intensity or spread. Studies have suggested that warming oceans may be altering wind patterns, moisture distribution, and the frequency of cloudbursts. Meanwhile, the Western Ghats, another major monsoon hotspot, appear to have drawn in more intense spells this year, redirecting the traditional balance of rainfall in India.
The implications of this deficit extend beyond meteorological records. Meghalaya, despite its reputation for excess rainfall, has long struggled with water scarcity. Cherrapunji itself, ironically, often suffers from acute drinking water shortages during the dry months. This is partly due to the region’s unique topography where rainwater rushes away through steep slopes, leaving little scope for natural storage. With the monsoon itself showing signs of weakening, the vulnerability of local populations could worsen. Agricultural cycles, forest health, and the flow of streams that sustain both biodiversity and human settlements are now at risk.
Furthermore, this shift disrupts cultural and ecological identities. Cherrapunji’s name is etched in collective memory as a symbol of nature’s abundance. Its waterfalls, such as Nohkalikai, swell each year into thunderous cascades, drawing visitors from around the globe. Its endless rains form the backdrop of folklore, songs, and even the ingenuity of the Khasi people, who constructed living root bridges that thrive in wet conditions. To imagine Sohra with dwindling rainfall is to question the very essence of its identity.
The anomaly of 2025 also raises questions about preparedness. With rainfall patterns becoming increasingly erratic, the reliance on traditional assumptions of monsoon behavior is no longer sufficient. The data from Sohra highlights the importance of diversifying water resources, improving storage, and integrating climate resilience into local planning. The paradox of a place drowning in rain for centuries yet parched in summers now risks being compounded by a new paradox: the wettest place on Earth drying up.
Yet, it is equally important to remember that this is not the end of Sohra’s story. The monsoon still has days left to redeem itself, and the skies over the Khasi Hills may yet open with renewed intensity before September draws to a close. Nature has a way of defying predictions, and Cherrapunji has surprised both skeptics and admirers before. Whether it breaks the record low or escapes narrowly, the 2025 monsoon will be remembered as a turning point—a year when the world paused to notice that even the clouds over Sohra can falter.
In the broader sense, this episode is a reminder of the fragility of climatic balance. The legends of Cherrapunji and Mawsynram were written by winds, hills, and oceans, but those forces themselves are now being rewritten by human actions and global changes. The rains may return with vigor in future years, restoring Sohra to its drenched glory, but the warning embedded in this year’s deficit is clear: no place, however exalted in natural abundance, is immune to the transformations of a warming world.
Cherrapunji’s skies may once again thunder with relentless downpours, but the question lingers—will it ever rain there as it once did, unceasing, unmeasured, and unchallenged?
(The writer can be reached at dipakkurmiglpltd@gmail.com)
