Climate
Why Is India Flooding If El Niño Predicted a Weak Monsoon?
El Niño was expected to suppress India’s 2026 monsoon, but July brought intense and uneven rainfall. While some regions remained deficient, extreme rain triggered floods and landslides across Assam, Gujarat, Odisha and Jammu & Kashmir. The pattern shows why seasonal rainfall averages alone cannot explain India’s increasingly erratic monsoon.
India entered the monsoon season with a warning: rainfall was expected to be below normal as El Niño conditions developed over the Pacific. Many feared water shortages and crop damages. The India Meteorological Department (IMD) forecast the June–September monsoon at 92% of the Long Period Average. The early monsoon appeared to follow that forecast. By June 30, India’s rainfall deficit had reached 40%. IMD also expected July rainfall to remain below normal.
But July turned the tables. Between July 1 and 26, India received 238.2 mm of rain against the normal 233.9 mm. By July 29, the national rainfall deficit had narrowed to 16%. Yet this was not a uniformly wet recovery. According to a report by Climate Trends, 17 states remained rainfall-deficient, while 15 recorded normal rainfall and four recorded excess or large-excess rainfall.
At the same time, extreme rainfall was triggering floods and landslides across several parts of the country, underscoring that the 2026 monsoon cannot be boiled down to a single rainfall number.
Two Sides of the Same Forecast
Assam offers the clearest example. East and Northeast India remained 30% below normal as of July 29. Yet Assam was facing severe flooding. By July 30, floods had affected more than 300,000 people and killed 78, while nearly 13,000 households remained without electricity.
The contradiction is important: a rainfall deficit at the seasonal or regional scale does not mean an absence of dangerous rainfall. Short, intense spells can produce flooding even when cumulative rainfall remains below normal.
Odisha tells a similar story. On July 16, IMD recorded extremely heavy rainfall of at least 21 cm in parts of the state, linked to a well-marked low-pressure area over the northwest Bay of Bengal and adjoining Odisha-West Bengal coast. IMD also warned of flash-flood risk in several districts. The system brought very heavy rain to Assam, Arunachal Pradesh and Bihar, with heavy rain across parts of Chhattisgarh, Madhya Pradesh, Nagaland and Tripura.
Then came Gujarat. On July 23, Valsad experienced an exceptional rainfall event, with Umergam recording 1,064 mm in 24 hours, according to the report analysed for this story. It was described as the third-highest 24-hour rainfall recorded in India since 1901. These events show that when rainfall arrives in increasingly concentrated bursts, it can trigger severe flooding and landslides even if seasonal totals remain normal or below average.
The South Tells Another Story
The picture changes across southern India. While July brought intense rainfall to parts of western, eastern and northeastern India, the South Peninsula—covering Kerala, Tamil Nadu, coastal and interior Karnataka, Andhra Pradesh and Telangana—remained 26% deficient as of July 29. Within this region, the shortfall was not uniform, with some coastal pockets receiving near-normal showers while interior districts continued to face prolonged dry spells. Northwest India was 10% deficient and Central India 1% deficient.
This geographical divide matters because it highlights how fragmented the monsoon has become at the sub-divisional level. India is not simply becoming wetter or drier overall. Instead, rainfall is increasingly uneven in both space and intensity, with some regions experiencing short bursts of destructive downpours while others remain locked in persistent deficits despite being in the same monsoon phase.
Why El Niño Did Not Tell the Whole Story
El Niño remains an important influence on the Indian monsoon, but scientists say it cannot be considered in isolation.
One factor is warming in the western Pacific. Former IMD Director General K J Ramesh said this has helped offset some of the rainfall-suppressing influence expected from El Niño. Cyclonic circulations moving through Myanmar have also sent remnants into the North Bay of Bengal, where they re-intensified and strengthened monsoon activity.
Western Disturbances have added another layer. Their increased interaction with the monsoon has contributed additional moisture from the Arabian Sea into Maharashtra and Gujarat and affected rainfall over the Himalayas and Northeast.
Jammu and Kashmir demonstrates how intense this interaction can become. During a July 19–24 rainfall spell, Reasi recorded 473.2 mm, followed by 417.5 mm in Udhampur and 349.9 mm in Rajouri. The rainfall triggered flash floods and landslides, with 28 deaths reported by July 21.
The issue, therefore, is not only how much rain falls. It is how quickly it falls and where it falls.
Climate change Adding Layers
Warmer oceans and land surfaces can increase the moisture available to favourable weather systems. Dr Akhil Srivastava of IMD said that when multiple monsoon systems develop under warmer conditions, they can gather more moisture and increase the likelihood of extreme rainfall.

This does not mean every flood can be directly attributed to climate change. Rather, climate change is altering the background conditions in which monsoon systems operate.
It is also changing the behaviour of Western Disturbances. Scientists cited in the report say changes in the subtropical westerly jet are allowing these systems to travel and oscillate differently during the monsoon season. Their interaction with the monsoon trough can contribute to heavier precipitation over northern India.
That matters for Himalayan states, where intense rainfall can quickly translate into flash floods and landslides.
The Unpredictable Monsoon Situation
This year’s monsoon is therefore more complicated than an El Niño-versus-rainfall equation. June delivered a 40% deficit. July then cut that deficit to 16%, but through highly uneven rainfall. Assam remained deficient while battling floods. Gujarat experienced an exceptional rainfall event. Odisha faced extreme rainfall linked to a Bay of Bengal low-pressure system. Jammu and Kashmir saw intense rain alongside flash floods and landslides. Meanwhile, the South Peninsula remained 26% deficient.
Phenomena like El Niño can no longer be applied uniformly to explain monsoon behaviour in a changing climate. The question is shifting from how much rain India receives over four months to where it falls, when it falls and how intensely it arrives.
For a country where agriculture, water storage, drainage, roads and disaster preparedness depend heavily on seasonal rainfall, that distinction matters. El Niño remains an important signal. But in a warming climate, it is only one part of a much larger system.
The biggest challenge India has to tackle is managing increasingly uneven and high-intensity rainfall rather than average seasonal totals. This calls for stronger real-time forecasting, district-level early warning systems, and climate-resilient infrastructure that can handle both flash floods and prolonged dry spells. Planning for monsoon risk must now shift from seasonal averages to managing extremes in space and time.
Climate
Record Drought and Extreme Heat Push European Rivers to Lows as Wildfires Spread North
The European drought is driving rivers to record lows as extreme heat, wildfires, crop losses and water shortages put Europe’s energy and transport systems under pressure.
A prolonged European drought combined with extreme heat is pushing major rivers to record lows, disrupting shipping and energy production while worsening crop losses and wildfire risks. As dry conditions spread north, Europe’s water, agriculture, ecosystems and public health systems are coming under increasing pressure.
A long period of low rainfall combined with extreme heatwaves has placed half of the European Union and the United Kingdom under drought conditions. A report published on August 12 by the European Commission Joint Research Centre and the European Drought Observatory reveals that nine percent of the region reached a critical alert level by late July.
Satellite data from Copernicus, the Earth monitoring program of the European Union, shows that severely dry soil is now damaging crops and plants across the continent. In its latest assessment, the observatory warned that “the drought has built up since early spring due to lower rainfall and higher than average temperatures, turning into fuel for devastating wildfires.”

European Drought Reaches Across the Continent
The lack of rain has driven four of Europe’s largest rivers—the Rhine, Danube, Loire, and Po—to dangerously low levels. Near Cologne, Germany, the Rhine fell to a fresh record low of 49 centimetres by mid-August, according to the Rhine Waterways and Shipping Authority — nearly 20 centimetres below the previous record of 68 centimetres set earlier in the summer, which had itself broken the prior all-time low recorded in 2018. Because large cargo boats need deeper water to float safely, operators have been forced to carry much lighter loads to avoid getting stuck on the riverbed, and in places river traffic has largely halted. Carrying smaller loads requires more trips, creating major shipping delays for important industrial materials across central Europe.
At the same time, low water levels and rising temperatures are creating a serious energy crisis across the continent. In France, power companies had to cut back nuclear energy production because river water became too warm to safely cool reactors without harming aquatic life. Hydroelectric power generation has also plunged across the Alps, northern Italy, and central-eastern Europe. Copernicus analysts noted that low river flows on the Danube are creating “serious operational challenges” for power plant cooling. In Italy’s Po Valley, the dried-out river basin has triggered a separate disaster: saltwater from the Adriatic Sea has flowed inland into depleted channels, ruining farmland soil and cutting off freshwater supplies for local crops.
Wildfires Burn Over 550,000 Hectares Across Europe
Dry plants and extreme heat have triggered widespread wildfires across the continent. According to August 11 data from the European Forest Fire Information System, 552,437 hectares of land have burned within the European Union since the start of the year, spread across 1,614 individual fires of 30 hectares or larger. Although this total remains below the 667,342 hectares burned by the same date in 2025 — a season that went on to become the worst on record for EU wildfires, with 1,034,552 hectares burned in total — it is significantly higher than the 20-year historical average.
Recent satellite data shows a clear shift: large wildfires are no longer staying just in southern hotspots like Spain and Greece. As dry weather pushes northward, fire risks are expanding into cooler regions, including northwestern France, southern Great Britain, the Alps, and the Balkans. Experts at the Joint Research Centre emphasized that “wildfire risk is no longer confined to southern Europe but is increasingly affecting wider parts of the continent under prolonged hot and dry conditions.”
Declining Harvests and Rising Health Risks
Continued heat and dry soil are dealing a heavy blow to European farmers. According to assessments by the European Joint Research Centre, crop yields across central and eastern Europe have dropped significantly. Production estimates for key spring and summer crops, such as grain maize and sunflowers, have fallen by six to seven percent. Winter crops have also suffered, with yield forecasts declining between one and four percent compared to earlier projections.
High temperatures are having a severe impact on human health as well. Monitoring data from public health agencies and the World Health Organization reveals a sharp surge in heat-related emergency admissions and deaths during extreme temperature episodes. Data compiled from national health agencies — including Germany’s Robert Koch Institute, which alone recorded an estimated 11,900 heat-linked deaths — put the region’s heat-related death toll above 25,000 as of early August, highlighting the severe human cost of this summer’s weather.
Seasonal Outlook and Emergency Response
Weather predictions indicate that dry conditions will continue through early autumn. According to the Copernicus Climate Change Service, drier and warmer weather is expected to persist across central-western Europe and southern Scandinavia through September. Climate experts also warn that a developing El Nino pattern could keep global temperatures higher than normal well into spring 2027. “Water resources, crops, energy systems, river transport, and ecosystems are all under growing pressure,” the report warned, with heatwave risks remaining high through August.
To coordinate emergency aid, the European Union activated its Civil Protection Mechanism. A dedicated fleet of 22 firefighting aircraft, 5 helicopters, and ground teams have been placed on standby across 12 countries. Meanwhile, the Copernicus satellite service has responded to more than 30 emergency requests since June, providing real-time mapping data to help local authorities track active fires and assess land damage on the ground.
Climate
Indigenous Peoples and Nature Conservation: What the Research Shows
Research shows that Indigenous Peoples and local communities play a significant role in protecting forests, biodiversity and carbon-rich ecosystems. Evidence suggests that secure land rights, traditional ecological knowledge and equitable participation in conservation governance can strengthen environmental outcomes.
Climate and biodiversity policies often focus on forests protected, carbon stored and species conserved. But an increasing body of research points to another factor that can influence these outcomes: who lives in, manages and makes decisions about ecologically important landscapes.
There are an estimated 476 million Indigenous Peoples across 90 countries, representing about 6.2% of the global population. Their territories overlap with many of the world’s remaining ecologically important landscapes, making their role increasingly relevant to climate and biodiversity policy.
The evidence does not support the blanket claim that Indigenous Peoples are inherently better conservationists. It does, however, show that land rights, ecological knowledge and meaningful participation in environmental governance can be important to conservation outcomes.
Indigenous Lands Overlap With Important Ecosystems
A 2018 study published in Nature Sustainability mapped Indigenous lands across 87 countries and politically distinct areas. It estimated that Indigenous Peoples manage or have tenure rights over at least 38 million sq km, more than one-quarter of the world’s terrestrial surface.
Their territories intersect approximately 40% of terrestrial protected areas and ecologically intact landscapes, including boreal and tropical primary forests, savannas and marshes.
The finding does not mean all Indigenous territories are pristine or formally protected. It demonstrates the substantial geographical overlap between Indigenous lands and landscapes that remain important for conservation.
That overlap matters for climate policy as well. Forests, wetlands and other intact ecosystems store carbon while supporting biodiversity and regulating water and other ecological processes.
One-third of Irrecoverable Carbon
The climate significance becomes clearer when carbon is considered.
A 2022 study in Nature Sustainability identified 139.1 gigatonnes of irrecoverable carbon remaining in Earth’s ecosystems, with considerable uncertainty around the estimate. The researchers found that 33.6% of this carbon—46.7 gigatonnes—is within lands managed by Indigenous Peoples and local communities, compared with 23% within protected areas.
“Irrecoverable” carbon refers to ecosystem carbon that, if released, could not be restored by mid-century—the timeframe considered critical for reaching net-zero emissions.
The figure does not mean Indigenous management itself creates these carbon stocks. It shows that a substantial share of carbon that climate policy has strong reason to protect is located within Indigenous and local-community lands.
Knowledge Accumulated Through Generations
Indigenous knowledge adds another dimension. Indigenous and local communities have developed detailed knowledge of species, habitats, seasonal cycles and natural resources through long-term relationships with particular landscapes. Such knowledge can complement scientific monitoring, particularly when environmental changes are observed over long periods.
The important question, however, is not simply whether conservation projects can use this knowledge. It is whether the people who hold it have a meaningful role in decisions affecting their territories.
A 2024 review in One Earth examined this question across conservation research. The researchers reviewed 648 empirical studies and analysed ecological outcomes in a subset of 170 studies. They found that more equitable governance arrangements—where Indigenous Peoples and local communities had equal partnership or primary control—were associated with significantly more positive ecological outcomes.
The study identifies an association, not proof that Indigenous governance automatically produces better results in every ecosystem. Conservation outcomes also depend on local institutions, ecological conditions, economic pressures and enforcement. But the finding challenges a model in which communities are merely consulted after conservation decisions have already been made.
The 30% Target Makes Governance Important
This issue is becoming more relevant as countries work towards the Kunming-Montreal Global Biodiversity Framework’s 30-by-30 target: conserving and effectively managing at least 30% of terrestrial, inland-water, coastal and marine areas by 2030.
The target itself calls for conservation areas to be equitably governed and recognises the rights of Indigenous Peoples and local communities where applicable. That means expanding protected areas cannot be measured only in hectares. How those areas are governed—and who has authority within them—also matters.
Climate Action Can Create New Pressures
The relationship between Indigenous territories and climate policy is not limited to forest conservation. The transition away from fossil fuels requires minerals used in batteries, electricity infrastructure and other technologies. Research published in Nature Sustainability found that more than half of the world’s energy-transition mineral resource base is located on or near the lands of Indigenous and peasant peoples.
This creates a potential contradiction: technologies intended to reduce emissions can generate new pressures on land and communities through mineral extraction.
A credible climate transition therefore has to consider not only the emissions avoided by new technologies, but also where their materials come from and whose territories are affected.
India: Where Forest Rights Meet Conservation
The global evidence has a clear relevance to India, although India’s legal framework generally uses the terms Scheduled Tribes and other traditional forest dwellers rather than the broader international category of Indigenous Peoples. India’s 2011 Census recorded about 104 million Scheduled Tribe people, representing 8.6% of the country’s population.

The Scheduled Tribes and Other Traditional Forest Dwellers (Recognition of Forest Rights) Act, 2006, commonly known as the Forest Rights Act, recognises rights of forest-dwelling Scheduled Tribes and other traditional forest dwellers over forest resources. It also provides for community forest-resource rights, including the right to protect, regenerate, conserve and manage community forest resources. Government data show the continuing scale of implementation.
As of December 31, 2025, the Ministry of Tribal Affairs reported 44,33,940 forest-rights claims had been settled, meaning a decision had been taken. These comprised 42,56,845 individual claims and 1,77,095 community claims. The data cover implementation in 20 states and one Union Territory.
The difference between individual and community claims is significant because community forest rights concern collective relationships with forests and their management. For India, therefore, the conservation question is not simply how much forest can be protected. It is also how communities with established relationships with forests participate in managing them and how their legally recognised rights are implemented.
What the Evidence Tells Us
The research does not justify portraying Indigenous Peoples as universally or inherently sustainable. Their communities, institutions and environmental practices differ widely. The evidence supports a more precise conclusion.
Indigenous Peoples manage or have tenure rights over at least 38 million sq km in the countries covered by the major global mapping study. Their territories intersect about 40% of terrestrial protected areas and ecologically intact landscapes. Indigenous Peoples and local communities manage lands containing 33.6% of the world’s mapped irrecoverable carbon. And a review of 648 conservation studies found that more equitable governance was associated with more positive ecological outcomes.
Together, these findings suggest that Indigenous Peoples should not be viewed simply as beneficiaries of conservation programmes or sources of traditional knowledge. They are already part of the governance of many ecologically important landscapes.
For climate and biodiversity policy, the implication is straightforward: protecting ecosystems can also require protecting the rights, knowledge and decision-making roles of the people who live with them. While that does not replace scientific research or environmental regulation. It expands the evidence and the institutions available to protect nature.
Climate
From Fighting Water to Saving It: The Netherlands Faces a Growing Drought Challenge
A land built to keep water out is now struggling to keep enough of it in — forcing a world leader in water management to rethink its infrastructure
The Netherlands built its global reputation by keeping water out. Now, longer dry spells and intensifying heatwaves are forcing the country to confront a very different problem: how to keep enough fresh water in the landscape. From greenhouse agriculture to homes built on wooden foundation piles, the Netherlands drought challenge is exposing the limits of infrastructure designed primarily for flood protection.
When people think of the Netherlands, the images that come to mind are windmills, tulip fields and the great sea walls that have kept the ocean at bay for centuries. The Dutch built their reputation, and much of their nation, on mastering water — pumping it away, holding it back, and reclaiming land from the sea to build a prosperous country on ground that, by rights, shouldn’t exist. Yet beneath that carefully engineered landscape, the Netherlands is now facing an unfamiliar problem: it is running out of fresh water.
As repeated summer heatwaves sweep across Western Europe, Dutch water authorities say they have reached the limit of what engineering can do. In several regions, officials have exhausted every standard measure available to them and are left with what amounts to a last resort — waiting, and hoping, for rain.
Netherlands Drought Challenge: From Floods to Water Scarcity
To understand how a country famous for its rainfall and rivers has arrived at this point, it helps to look at how the land itself was designed. For generations, the Dutch water system had one job: get excess water out to sea as fast as possible, to prevent flooding. That same efficiency has become a liability as weather patterns shift towards longer dry spells and more intense heat. The pressure peaks in late summer, when temperatures regularly cross 35°C and water evaporates faster than rainfall can replace it.
The consequences of shrinking water reserves go well beyond the daily weather report. They are already reaching into the economy, and into the foundations — quite literally — of Dutch homes.
Thousands of historic Dutch houses stand on wooden foundation piles. When groundwater levels drop, those piles are exposed to air and begin to rot. On clay and peat soils, the ground shrinks unevenly, pulling foundations down and cracking brick walls
Economic Strain and Sinking Homes
In Westland, the heart of Dutch greenhouse horticulture, the Delfland water authority has banned growers from drawing irrigation water from local ditches and canals — the first such ban in its history. According to the growers’ umbrella body Glastuinbouw Nederland, the ban affects around 150 commercial growers, with potential damages running as high as €150 million.
At the same time, a quieter crisis is unfolding beneath people’s homes. Thousands of historic Dutch houses stand on wooden foundation piles. When groundwater levels drop, those piles are exposed to air and begin to rot. On clay and peat soils, the ground shrinks unevenly, pulling foundations down and cracking brick walls. The Council for the Living Environment and Infrastructure estimates that close to half a million buildings across the country could show foundation damage by 2035, with repair costs reaching as much as €54 billion.
From Water Battle to Water Sponge
This reality is forcing a fundamental shift in how the Netherlands manages its resources. For centuries, Dutch policy was simple: fight the water, and push it away. Today, water authorities are engaged in a delicate balancing act, trying to save every drop using canal locks and storage basins. But holding onto existing water can only do so much once the rain stops altogether.
Long-term resilience will require redesigning the landscape itself. Rather than treating rainwater as a threat to be flushed out to sea, experts increasingly argue that the Netherlands needs to function more like a giant sponge — capturing heavy winter rain and storing it safely to survive the dry summer months that are becoming the norm.
A Lesson Beyond Borders
What is unfolding in the Netherlands carries a lesson well beyond it. If a nation this experienced in water engineering is struggling to keep pace with a changing climate, it says something about how quickly conditions can outrun even the most sophisticated infrastructure. As riverbeds stay low and the dry spells drag on, the Dutch find themselves in an unfamiliar position for a country built on water: waiting for the skies to open.
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