New Delhi: By late May, Delhi feels like a furnace. Roads shimmer under the afternoon glare, metro pillars radiate heat long after sunset, and even pockets of city forests seem to exhale warmth.Across northwest India, temperatures push past 45°C, bringing heatstroke warnings, water stress and exhausted streets. Each summer, the same question returns: How can this level of heat possibly be normal?Yet, beyond the panic of shooting temperatures, meteorologists, foresters, ecologists and agricultural scientists point to a more complicated truth. There is a purpose to the brutal summer. It is also part of an engine that kills pests, aids soil, ripens fruits, and importantly, drives the monsoon. The same heat that scorches the plains helps create pressure gradients that pull rain-bearing winds over the subcontinent.The Indian monsoon is often described simply as seasonal rain. In reality, it behaves more like a continental-scale breathing system. During May and June, the landmass over Rajasthan, Delhi, Haryana and Pakistan heats much faster than the surrounding Indian Ocean. As the ground bakes under relentless sunlight, hot air rises rapidly, creating an enormous low-pressure zone over northwest India. Meteorologists call this the “heat low”.This low-pressure region acts almost like an atmospheric vacuum. Moisture-laden winds from Arabian Sea and Bay of Bengal rush towards it, eventually colliding with the cooler upper air and producing monsoon rainfall. In simple terms, the land must become hot before ocean winds can surge inland carrying rain.Prof Manju Mohan of Centre for Atmospheric Sciences at Indian Institute of Technology-Delhi explains how summer heat creates convection currents that strengthen monsoon circulation. “Air flows from high pressure to low pressure. The higher the temperature and stronger the pressure gradients, the stronger the circulation becomes. When moisture-carrying winds rush in to fill this low-pressure gap, rainfall occurs,” she says.However, Mohan cautions that heatwaves are dangerous, especially for outdoor workers and the vulnerable communities. But scientifically, the intense summer heating is part of the seasonal transition that “paves the way” for the monsoon.This process is incredibly harsh on northwest India because it is landlocked and dry. Unlike coastal cities moderated by sea winds, Delhi and its surrounding regions absorb and retain heat rapidly. Hot winds sweeping in from Thar Desert further intensify temperatures.“This heat can’t be separated from the monsoon. Extreme heating over northwest India helps pull monsoon currents inland,” says meteorologist Mahesh Palawat of Skymet.But the effects of summer extend beyond meteorology. Across forests and grasslands, wildlife species have evolved around these cycles of heat, scarcity and renewal.Ujjwal Kumar, research scientist at Wildlife Institute of India, Dehradun, notes that many animals begin seasonal movement patterns during the extreme summer. In central Indian forests and hill ecosystems, water availability declines sharply by late winter and early summer, pushing species such as gaur, sambar deer and even predators towards lower plains where water remains available. “For social animals, staying together also reduces individual-level predation risk,” he says.At the same time, summer-fruiting trees, such as mahua, tendu, jamun and ber, become critical nutritional sources. “For many herbivores, especially ungulates, which rely on cellulose, the seeds of these fruits are a major source of protein and energy,” Kumar says, adding that when the monsoon finally arrives, fresh forage spreads rapidly across forests and grasslands, triggering what ecologists often describe as a “seasonal feast” during reverse migration.Scientists explain how modern soil management adapts to the harsh summers instead of fighting nature — using cover crops and organic biomass to protect and enrich the soil.“Extreme summer temperatures can damage the soil’s organic carbon and microbial life if fields are left bare. But with conservation practices like crop residue cover, green manuring and planting short-duration legumes, such as moong or dhaincha, heat turns into an advantage by improving soil health, moisture retention and nutrient cycling,” says Dr B S Dwivedi, secretary, National Academy of Agricultural Sciences.Farming, too, depends on this punishing interval between spring and rain. Scientists at Indian Agricultural Research Institute say the intense summer heat naturally suppresses several fungal diseases and insect populations, reduces the viability of many weed seeds and disease-causing spores before the kharif sowing season begins.The scorching Zaid season of May and June also supports crops, such as fodder and moong pulses, while some mango varieties require sustained heat for proper ripening. “Summers are punishing but they are also agriculturally functional,” according to Dwivedi.Ecologists argue that even on a planetary scale, summer heat reflects something fundamental about how life on Earth operates.Faiyaz Khudsar, scientist-in-charge of Delhi Development Authority Biodiversity Parks Programme, says solar radiation continuously powers the ecological systems humans depend on. Sunlight drives photosynthesis, atmospheric circulation, ocean currents and hydrological cycle. Without sustained solar heating, rainfall systems will weaken, nutrient cycles stagnate and ecosystems across land and sea collapse.None of this undermines the suffering of a Delhi summer as longer heatwaves are more erratic, with health experts warning that rising urban temperatures, concrete expansion and humidity are pushing human tolerance limits.However, beyond the suffering in the capital’s concrete heat islands, India’s pre-monsoon heat is part of a climatic engine that shapes rivers, crops, forests, migration patterns and civilisations.
