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The wildfires, floods, and heatwaves: Understanding the science behind climate change

The stories we tell today will define the world that future generations inherit. Will they look back and see a world that acted in time, or a world that failed to change until it was too late?

Image credit: Gerd Altmann from Pixabay
Dipin Damodharan

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In the heart of the Amazon rainforest, one of the most biodiverse places on Earth, a massive wildfire raged through the thick, lush greenery. This wasn’t just any fire; it was a calamity that consumed more than 17 million animals in its path, a chilling reminder of how the destruction of nature can reverberate across ecosystems. The Amazon, often referred to as the “lungs of the Earth,” plays a pivotal role in managing the planet’s climate. Yet, the actions of humanity—deforestation, illegal logging, and deliberate fires for agricultural purposes—have not only caused immeasurable loss to wildlife but have also accelerated climate change. The forest’s destruction led to a dangerous feedback loop, intensifying global weather patterns in ways that humans had never anticipated.

Fast forward to 2018, and the monsoon rains that battered Kerala, a state in India, were an equally dire omen. What began as an ordinary August downpour escalated into one of the deadliest floods in the region in almost a century. Rivers overflowed, breaking through dams and inundating vast swathes of land. Entire towns were submerged. Hundreds of lives were lost, and the devastation reached far beyond the physical damage, triggering social and economic upheaval. The aftermath left thousands homeless, as people sought refuge in makeshift shelters. The floods in Kerala were not an isolated incident; in fact, they were a warning from nature, signaling a world grappling with extreme weather events, made worse by human-induced climate change. The same was the case with 2024 Wayanad landslides.

And this global pattern of violent weather doesn’t stop in the tropics. In recent years, a blistering heatwave has swept across parts of North America. The US and Canada, known for their cold winters, have experienced record-breaking summer temperatures, an anomaly that scientists have linked directly to climate change. Oregon, once known for its temperate weather, saw the largest wildfire in its history, spurred by the heatwave. This was not just a local disaster—it was part of a larger, worrying trend in which global warming is creating the conditions for wildfires, floods, and heatwaves to proliferate at an unprecedented rate.

Climate change refers to significant, long-term shifts in weather patterns and temperatures.

These are not just isolated incidents. They are signs of a planet in distress, a planet experiencing the devastating effects of climate change, a phenomenon that is rapidly altering our environment and our lives.

The Science Behind the Crisis

Climate change refers to significant, long-term shifts in weather patterns and temperatures. These changes can manifest in a variety of ways: from prolonged droughts and unseasonal rains to extreme heatwaves and hurricanes. The root cause of today’s accelerated climate change is primarily human activity, particularly the burning of fossil fuels, deforestation, and industrial emissions, which release greenhouse gases like carbon dioxide into the atmosphere.

The Earth’s climate has always undergone natural variations—shifting from ice ages to warmer periods over millennia. However, what we are witnessing today is a much more rapid and intense change, driven by human actions. According to scientists, the Earth’s average temperature has risen by approximately 1.1°C since the late 19th century, with the past few decades seeing a rate of warming unprecedented in the geological record. The current trajectory suggests that global temperatures could rise by another 1-2°C by the end of the century, which would have catastrophic implications for both human and natural systems.

The impacts of this warming are already being felt globally. Melting ice caps and glaciers, rising sea levels, shifting weather patterns, and more frequent extreme weather events are some of the most visible signs. The Amazon rainforest, which once functioned as a massive carbon sink, is now a source of carbon emissions due to deforestation and wildfires. Meanwhile, heatwaves in parts of Europe and North America have reached previously unimaginable levels, set new temperature records and causing widespread harm.

A Global Phenomenon: From Kerala to Oregon

The devastating Kerala floods of 2018 were preceded by a series of warnings. The state’s weather patterns had been shifting, with increasingly unpredictable rainfall, leading to swollen rivers and the overflowing of dams. Once a relatively regular occurrence, floods in Kerala became more intense and frequent over time. Experts argue that climate change, through the intensification of the monsoon season and rising sea levels, has exacerbated the situation. But Kerala is not alone. Across the world, regions that were once resilient to extreme weather are now facing unprecedented levels of flooding, wildfires, and other disasters.

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Image: Dominic Wunderlich from Pixabay

In 2020, when a record heatwave struck North America, temperatures in the Pacific Northwest soared to levels never seen before. Oregon, a state known for its temperate climate, reported its highest-ever temperatures. This heatwave triggered wildfires that devastated millions of acres of forest and caused significant loss of life. The fires were not simply a result of hot weather, but of the conditions created by climate change—dry forests, extreme heat, and shifting weather patterns all came together to fuel the fires.

Similarly, across the Atlantic, parts of Europe experienced an unusually harsh summer, with wildfires ravaging Spain, Portugal, and southern France. These fires were not natural events but were made more intense by the warming climate. Even in regions like Siberia, where wildfires were once rare, extreme temperatures and dry conditions have now turned vast areas into tinderboxes.

The Growing Threat: What the Future Holds

The world’s climate is now so volatile that extreme weather events are no longer an anomaly. They are becoming the new normal. Rising temperatures are leading to extreme heatwaves, higher sea levels are threatening coastal communities, and shifting weather patterns are disrupting ecosystems and agriculture. We are seeing longer droughts, more intense storms, and unpredictable rainfall, all of which are affecting millions of people across the globe.

In the coming decades, the situation is expected to worsen. According to scientists, we are on track to exceed a 1.5°C rise in global temperatures by 2050, with the potential for far-reaching consequences. Sea levels are projected to rise, displacing millions of people, while agriculture will suffer due to unpredictable rainfall and extreme temperatures. Already vulnerable regions, such as the Pacific Islands, will be the hardest hit, while major cities like New York, Mumbai, and Jakarta are all at risk of flooding.

Rising Temperatures and Their Far-reaching Effects

Even small changes in the Earth’s temperature can have profound impacts. A temperature-increase of just 1.5°C could lead to the irreversible melting of polar ice caps, resulting in a rise in sea levels that would submerge entire cities. Rising temperatures can also trigger the release of methane from thawing permafrost, a potent greenhouse gas that could accelerate global warming even further.

The stories from the Amazon, Kerala, Oregon, and beyond serve as stark reminders that the climate crisis is not a future problem—it is a present-day reality

One of the most troubling aspects of this warming is how it is changing the planet’s ecosystems. Species that once thrived in specific temperature ranges are now struggling to survive. Many are migrating to cooler areas, while others face extinction. As habitats shrink and weather patterns change, the very fabric of biodiversity is at risk.

Can We Change Course?

The question now is: Can we reverse or at least slow down these changes? While the situation is dire, scientists and environmentalists believe that immediate action can still mitigate the worst impacts of climate change. Transitioning to renewable energy sources, reducing deforestation, and investing in sustainable agricultural practices are essential steps. Governments, corporations, and individuals all have a role to play in ensuring that we shift towards a more sustainable and resilient future.

There is still time to act, but the window is closing fast. The more we delay, the more severe the impacts will be. The stories from the Amazon, Kerala, Oregon, and beyond serve as stark reminders that the climate crisis is not a future problem—it is a present-day reality that we can no longer afford to ignore.

A Global Call to Action

From the scorched rainforests of the Amazon to the flooded streets of Kerala and the heat-baked forests of Oregon, climate change is no longer a distant concept. It is here, now, and it affects all of us. But the power to change our future lies in our hands. By making sustainable choices, demanding policy changes, and holding accountable those who contribute to the climate crisis, we can begin to heal our planet before it’s too late.

The stories we tell today will define the world that future generations inherit. Will they look back and see a world that acted in time, or a world that failed to change until it was too late? The choice is ours.

Dipin Damodharan is an award-winning journalist, editor and media entrepreneur, and Co-founder and Editor-in-Chief of EdPublica, an independent global media platform covering education, science, research, innovation, climate and public policy. With more than a decade of experience in journalism, he has worked across print, digital and multimedia media. His reporting explores science, climate, sustainability and the social impact of research and innovation. His work has been recognised by the Solutions Journalism Network and other journalism organisations.

Earth

Greener Forests, Weaker Carbon Sinks? Study Finds Declining Productivity in Northeast India

A 24-year satellite-based study finds that Northeast India’s forests are experiencing declining carbon productivity despite relatively stable canopy cover, highlighting how rising atmospheric dryness could weaken their capacity to absorb and retain carbon.

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Dense green forest canopy with sunlight filtering through the leaves of tall trees.
A dense forest canopy illustrating the vegetation cover and ecological richness of tropical forest ecosystems.Image credit:Pexels

Forests in Northeast India are showing signs of a weakening capacity to accumulate carbon despite maintaining relatively stable canopy cover, according to a study published in Ecological Indicators in October 2026. The research suggests that increasing vegetation greenness does not necessarily indicate stronger carbon sinks, highlighting the need to assess forest health beyond satellite measurements of green cover.

Titled Are Greener Forests Stronger Carbon Sinks? Rising Vapour Pressure Deficit Instigates Greening-Productivity Decoupling in a Tropical Biodiversity Hotspot in India, the study examined forest carbon dynamics across Northeast India using 24 years of satellite-derived data from 2001 to 2024.

Researchers analysed three indicators: Leaf Area Index (LAI), Gross Primary Productivity (GPP) and Net Primary Productivity (NPP). These measurements helped assess changes in forest canopy structure, photosynthetic activity and the amount of carbon retained in plant biomass after accounting for plant respiration.

The analysis found that while canopy structure remained relatively stable and gross primary productivity increased modestly by 1.76 grams of carbon per square metre annually, net primary productivity declined by 0.83 grams of carbon per square metre annually across much of the region.

The researchers identified a divergence between canopy greenness and carbon productivity across approximately 40% of forested areas. A separate divergence between photosynthetic activity and net productivity was observed across around 30% of the region.

These findings indicate that forests can maintain their green appearance without achieving corresponding gains in carbon accumulation.

Atmospheric dryness emerges as a major factor

The study identified rising Vapour Pressure Deficit (VPD) as a primary driver of declining forest productivity. VPD measures the difference between the amount of moisture the atmosphere can hold and the moisture it actually contains. Higher VPD indicates greater atmospheric demand for water, increasing stress on vegetation.

Under such conditions, plants may close their stomata, the small pores on their leaves, to reduce water loss. This also restricts the intake of carbon dioxide required for photosynthesis, potentially reducing the amount of carbon absorbed by vegetation.

The researchers also identified a major shift in forest carbon functioning beginning around 2012. Their analysis suggests that the relationship between canopy structure, photosynthesis and net carbon accumulation has weakened over time.

The findings are particularly significant for Northeast India, which the study identifies as a climatically sensitive biodiversity hotspot containing approximately one-third of India’s forest carbon.

Earlier research points to similar concerns

The findings build on earlier research published in Scientific Reports in December 2023, which examined vegetation productivity across India between 2001 and 2019.

That study found that India’s Leaf Area Index increased by 6.75% in consistently forested areas, while Net Primary Productivity declined by 6.19%. Northeast India, the Western Ghats and parts of Peninsular India emerged as important regions experiencing declining productivity.

The 2023 research associated these changes with rising temperatures, which can reduce photosynthesis and increase plant respiration beyond certain temperature thresholds.

Another study examining a semi-deciduous forest in Kaziranga, published in Agricultural and Forest Meteorology in 2022, demonstrated how carbon exchange varies with seasonal and climatic conditions. It found that the forest functioned as a carbon sink during the pre-monsoon season but as a carbon source during winter in the observed study period.

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Image of a dense forest alongside a flowing river.Image credit:Pexels

Together, these studies highlight the importance of examining forest productivity, atmospheric conditions and seasonal carbon exchange rather than relying solely on changes in green cover.

The latest research does not suggest that Northeast India’s forests are structurally collapsing. Instead, it points to a less visible change in their ecological functioning, with implications for forest carbon accounting and climate-resilient forest management.

The findings underline the need for monitoring systems that combine satellite observations with measurements of atmospheric stress and carbon productivity to better understand how tropical forests respond to a warming climate.

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Earth

252 Million Hectares Under Restoration Across 149 Countries, but UN Warns of 2030 Target Gap

A UN report finds that 252 million hectares across 149 countries are under ecosystem restoration. However, increased investment and accelerated action are needed to meet global restoration targets by 2030.

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River flowing through a forested mountain landscape with evergreen trees and snow-covered peaks.
Healthy mountain forests and river ecosystems play an important role in maintaining biodiversity and ecological balance.Image credit:Pexels

Global efforts to restore degraded ecosystems have reached 252 million hectares across 149 countries, generating more than one million green jobs. However, a new United Nations assessment warns that restoration efforts remain insufficient to meet international biodiversity targets by 2030, calling for a more than fourfold increase in annual investment.

The findings are presented in the Restoration Progress Report: Nature’s Comeback – Scaling Ecosystem Restoration for People and Planet, released on October 29, 2026, by the United Nations Environment Programme (UNEP), the Food and Agriculture Organization (FAO) and the Secretariat of the Convention on Biological Diversity (CBD).

The report provides the first comprehensive global assessment of progress towards commitments to restore approximately one billion hectares of degraded ecosystems. These commitments are linked to the UN Decade on Ecosystem Restoration (2021–2030) and the Kunming-Montreal Global Biodiversity Framework, which calls for at least 30 per cent of degraded terrestrial, freshwater, marine and coastal ecosystems to be under effective restoration by 2030.

According to the assessment, the 252 million hectares currently documented under restoration represent the largest recorded global restoration effort. However, this accounts for only 34 per cent of the indicative global benchmark associated with the 2030 target.

Freshwater and marine ecosystems lag behind

The report identifies considerable differences in restoration progress across regions and ecosystem types. Asia accounts for the largest share of documented restoration, with 192.2 million hectares, followed by Africa with 36.3 million hectares and Europe with 9.1 million hectares. North and Central America account for 5.8 million hectares, South America 5.4 million hectares and Oceania 3.2 million hectares.

However, the report cautions that these figures should not be interpreted as a ranking of restoration performance, as they also reflect differences in regional land area and monitoring and reporting capacities.

Restoration of terrestrial ecosystems has reached nearly half of the global 2030 target. China reports the largest terrestrial restoration area, with 127.4 million hectares, while substantial restoration activities have also been documented in Mongolia and Kazakhstan.

Progress remains considerably slower in freshwater, marine and coastal ecosystems, despite these environments experiencing rapid degradation.

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A river along the side of a dense forest. Image credit: Pexels

The assessment documents 11 million hectares of freshwater ecosystems under restoration across 62 countries and 5.7 million hectares of marine and coastal ecosystems across 46 countries. The report also notes that limited monitoring and reporting may mean that actual restoration activities in these ecosystems are higher than the documented figures.

Meanwhile, the share of countries reporting implemented wetland restoration or rehabilitation programmes has increased from 8 per cent in 2022 to 54 per cent.

Restoration financing needs to increase fourfold

Insufficient investment remains a major obstacle to achieving global restoration commitments. The report estimates that annual restoration financing must increase from US$64 billion to US$296 billion by 2030, representing more than a fourfold rise.

Agroforestry requires the largest estimated annual investment, at US$87 billion, followed by restorative reforestation at US$52 billion, peatland restoration at US$44 billion and seagrass restoration at US$28 billion.

The report identifies employment generation as another potential benefit of scaling up restoration. While more than one million green jobs have already been associated with restoration initiatives, increased global investment could generate up to 32 million additional jobs by 2030.

It also highlights the potential contribution of ecosystem restoration to climate mitigation and biodiversity protection. Research cited in the assessment indicates that restoring just 15 per cent of global priority areas could capture and store 30 per cent of carbon dioxide-equivalent emissions released since the Industrial Revolution and help prevent 60 per cent of projected species extinctions.

The report further identifies the participation and leadership of Indigenous Peoples and local communities as essential to ensuring long-term restoration outcomes. Secure land rights, stronger monitoring systems and sustained political commitment are among the priorities identified.

With five years remaining in the UN Decade on Ecosystem Restoration, the assessment calls on governments to move beyond isolated restoration projects towards coordinated, long-term programmes that address the underlying causes of ecosystem degradation.

It emphasises that the 2030 targets should serve as a milestone in the restoration process rather than its conclusion, as ecological recovery requires sustained action and investment beyond the end of the decade.

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Climate & Environment

Kashmir’s Traditional Rice Varieties Hold Genetic Clues to Climate Resilience

A new study by SKUAST-Kashmir researchers identifies cold-tolerance genes in traditional rice varieties, highlighting their potential for climate-resilient crop breeding.

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Farmers transplanting young rice seedlings in a flooded paddy field.
Traditional rice cultivation highlights the agricultural heritage that researchers are working to preserve as they investigate genetic resources for climate-resilient crops.Imagecredit:Pexels

For generations, farmers in Kashmir have cultivated traditional varieties of rice adapted to the region’s distinctive growing conditions. A new genomic study has found that these varieties retain genetic characteristics associated with cold tolerance and local adaptation, potentially offering valuable resources for developing climate-resilient crops.

Researchers at the Sher-e-Kashmir University of Agricultural Sciences and Technology of Kashmir (SKUAST-Kashmir), Srinagar, analysed 142 rice germplasm samples to examine the genetic diversity and evolutionary history of rice cultivated in the region. Published in The Plant Genome in 2026, the study identified genetic signatures in traditional varieties that could help researchers develop rice better suited to environmental stress.

The findings are significant as climate change alters growing conditions and increases uncertainty for agricultural production. Preserving traditional crop varieties could give plant breeders access to genetic traits that may have become less common in modern cultivars.

Genes linked to cold tolerance

The study, titled Re-sequencing 142 rice genomes reveals the fine-scale population structure and phylogenetic affinities of landraces of Kashmir Valley: Evidence from domestication and adaptive signatures, used genomic analysis to investigate relationships among traditional landraces, modern varieties and other rice genetic resources.

The researchers found that Kashmir’s traditional varieties carried genetic signatures associated with temperate japonica rice, while many modern varieties showed stronger associations with indica lineages from subtropical India. This distinction points to differences in their genetic histories and adaptation to local growing environments.

Among the important findings was the identification of favourable variants of CTB4a and HAN1, two genes associated with cold tolerance in rice. The researchers also examined genetic variation linked to grain quality, plant development and other agricultural traits.

Traditional varieties, including Mushq Budji, Kamad, Kaw Kreer, Nun Beoul and Zag, displayed distinctive genetic patterns. Their diversity could provide useful material for future crop-improvement programmes.

The findings do not establish that all these varieties are more resilient than modern cultivars under every environmental condition. Instead, they identify genetic resources that warrant further investigation through breeding programmes and field trials.

Earlier research explains the significance

Previous research provides a scientific basis for investigating the cold-tolerance genes identified in Kashmir’s traditional rice varieties.

A 2017 study published in Nature Communications examined CTB4a, a gene associated with cold tolerance during the booting stage of rice development, when reproductive structures form. The researchers found that a favourable variant improved cold tolerance and helped maintain pollen fertility and seed setting under low-temperature conditions.

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Crops in a paddy field.Image credit:Pexels

Similarly, a 2019 study published in the Proceedings of the National Academy of Sciences investigated HAN1 and found that natural genetic variation in the gene contributes to chilling tolerance in temperate japonica rice. The findings helped explain how rice adapted to cooler climates.

These studies strengthen the case for investigating CTB4a and HAN1 variants in Kashmir’s rice germplasm. However, the presence of promising genetic variants does not automatically guarantee improved performance in farmers’ fields. Their effects can depend on the crop’s broader genetic background, the timing and intensity of temperature stress, and other environmental conditions.

Conserving agricultural diversity

The Kashmir study also offers insights into the region’s agricultural history. Its genetic analysis suggests links between traditional Kashmir rice varieties and temperate rice lineages associated with Northeast Asia. The researchers propose that these lineages reached the region after approximately 1500 BCE, although this historical reconstruction remains an interpretation of genetic and archaeological evidence.

Beyond their historical significance, traditional rice varieties may preserve traits useful for future agricultural challenges. Modern breeding programmes often prioritise yield and other selected characteristics, but genetic diversity within traditional varieties can provide additional options for addressing environmental stress and maintaining grain quality.

The findings underline the importance of conserving traditional rice germplasm in gene banks and supporting its continued cultivation where feasible. Such conservation helps prevent potentially valuable genetic material from disappearing as farming systems and crop preferences change.

As climate change places increasing pressure on agricultural systems, Kashmir’s traditional rice varieties offer researchers a valuable starting point for investigating crop adaptation. Their genetic diversity connects generations of farming knowledge with modern genomic research, potentially helping plant breeders develop rice varieties suited to changing environmental conditions while preserving the region’s agricultural heritage.

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