The frequency and intensity of extreme weather events have surged dramatically in recent years. From devastating floods and wildfires to unprecedented heatwaves and hurricanes, these events are reshaping landscapes, displacing communities, and straining resources worldwide. But what connects all these seemingly unrelated disasters? The answer lies in a warming planet driven by industrial activities and the resulting destabilization of Earth’s climate system.

Table of Contents

Industrial activities and climate destabilization

Human activities are increasing the amount of heat-trapping greenhouse gases in the atmosphere, causing the Earth to warm at an unprecedented rate. The burning of fossil fuels, deforestation, and agricultural practices release massive quantities of carbon dioxide, methane, and nitrous oxide into the atmosphere. Atmospheric concentrations of carbon dioxide are now at the highest levels in the last 800,000 years.

These industrial and agricultural activities are the primary drivers of climate destabilization. Greenhouse gases emitted by human activities alter Earth’s energy balance and thus its climate. Scientists have established beyond reasonable doubt that this alteration is the fundamental reason behind the increasing frequency and severity of extreme weather events globally.

Climate system dynamics and energy balance

Understanding why greenhouse gas emissions lead to extreme weather requires grasping how Earth’s climate system maintains its energy balance. Earth’s temperature depends on the balance between incoming energy from the sun and outgoing energy radiated back to space.

The natural greenhouse effect

When sunlight reaches Earth’s surface, some is reflected back to space while the rest is absorbed, warming the planet. The Earth then re-emits this energy as infrared radiation. Greenhouse gases trap this outgoing heat near Earth’s surface, acting like a blanket that keeps temperatures warmer than they would otherwise be.

This natural greenhouse effect maintains Earth’s average surface temperature at approximately 15ยฐC (59ยฐF), which is essential for supporting life. Without the greenhouse effect, Earth’s average temperature would be about -18ยฐC, far too cold for liquid water or life as we know it.

Disrupting the balance

Adding more greenhouse gases to the atmosphere makes it even more effective at preventing heat from escaping into space. When less energy leaves than enters the system, Earth warms until a new balance is established. The current energy imbalance is approximately 0.8 watts per square meter, meaning Earth is continuously accumulating heat.

This addition of carbon dioxide to the atmosphere is known as climate forcing, as it destabilizes Earth’s temperature. The consequence is global warming and increasingly volatile weather patterns.

Accelerating hydrological cycles

One of the most significant consequences of global warming is the acceleration of the hydrological cycle. Climate change is causing parts of the water cycle to speed up as warming global temperatures increase the rate of evaporation worldwide. This acceleration has cascading effects throughout Earth’s climate system.

More evaporation, more extreme precipitation

A warmer atmosphere holds more water vapor. Warmer air can hold more moisture than cool air, so the air sucks up more water from oceans, lakes, soil, and plants. When this moisture-laden air cools, it releases more intense precipitation.

Global warming can alter the hydrological cycle in various forms, leading to more intensive and frequent precipitation extreme events such as droughts, storms, and floods. The increased atmospheric moisture content causes precipitation events to change in intensity, frequency, and duration, with global precipitation increasing by 2-3 percent for every degree Celsius of warming.

Rising sea levels

The accelerated hydrological cycle contributes to sea level rise through two primary mechanisms. First, water from melting glaciers and ice sheets flows into the ocean. Second, ocean water expands as it warms.

As of the 2020s, sea levels are 0.10-0.20 meters higher than a century ago due to climate change, and could rise as much as 1.1 meters by 2100 if greenhouse gas emissions continue at projected levels. This rise threatens coastal communities and infrastructure worldwide.

Glacier retreat and altered precipitation patterns

The frozen parts of Earth’s surface are melting at alarming rates. Mountain glaciers, Arctic ice, and polar ice sheets have all decreased significantly. Changes in precipitation patterns are also occurring, with some regions experiencing more evaporation and others receiving altered seasonal rainfall.

The evidence: extreme events in recent years

The connection between climate change and extreme weather is no longer theoretical. In 2024, climate change contributed to the deaths of at least 3,700 people and the displacement of millions in 26 weather events studied by World Weather Attribution. These represented just a fraction of the 219 extreme events that met their assessment criteria.

Record-breaking impacts

Extreme weather events in 2024 led to the highest number of new displacements recorded in the past 16 years. A total of 605 extreme weather events occurred globally in 2024, with 148 classified as unprecedented and 289 as unusual.

In the United States alone, there were 27 disasters in 2024 that individually cost $1 billion or more, the second-highest number since record-keeping began in 1980. The average time between billion-dollar disasters in 2024 was just 12 days, compared to 82 days in the early 1980s.

Floods and rainfall intensification

Of the 16 major floods studied in 2024, 15 were driven by climate change-amplified rainfall. This reflects fundamental physics: a warmer atmosphere holds more moisture, producing heavier downpours. From Dubai to Rio Grande do Sul to the Southern Appalachians, devastating floods marked the year.

Heat and drought

Climate change added an average of 41 additional days of dangerous heat globally in 2024. Worsening heat waves are the most direct consequence of pumping climate-warming pollution into the atmosphere, increasing average temperatures worldwide and making extreme heat events hotter and more frequent.

Data challenges in climate research

Despite the clear evidence linking climate change to extreme events, researchers face significant challenges in analyzing long-term trends. Understanding how extreme events are changing requires extensive historical data, which is often unavailable or incomplete.

Limited historical records

Climate scientists require observational records that are long and free from significant gaps, major errors, and inhomogeneities. While at least 30 years of records are typically needed to establish meaningful climate baselines, many regions lack such comprehensive data. The question of effective management of observational data remains a major problem in many developing countries.

Disparities in data coverage

Data coverage is often sparser in developing countries and vulnerable regions, which are often most at risk from climate change. This data scarcity hinders effective adaptation planning and resource allocation precisely where it is most needed. In many developing countries, systematic collection of temperature and precipitation data only began after World War II.

Data rescue and digitization efforts

Historical climate records in many regions exist largely in hardcopy manuscript form, making them difficult to use and at risk of permanent loss. The World Meteorological Organization has supported data rescue and digitization efforts, particularly in developing countries, to preserve these valuable records. Initiatives like ENACTS are working to improve the availability and quality of climate data in Africa by combining station observations with satellite estimates.

Why data gaps matter

These data limitations have practical consequences for understanding and responding to climate change. Attribution studies have sometimes been unable to quantify climate change’s influence on extreme events due to lack of weather data and limitations in climate models. Improved monitoring and data sharing are essential for developing accurate projections and effective adaptation strategies.

Looking ahead: the urgency of action

The clear signs of human-induced climate change reached new heights in 2024, with some consequences being irreversible over hundreds or thousands of years. 2024 was likely the first calendar year to exceed 1.5ยฐC above pre-industrial levels.

As greenhouse gas concentrations continue rising, the energy imbalance will grow, and extreme weather will intensify. As long as greenhouse gas concentrations continue to rise, the amount of absorbed solar energy will continue to exceed the amount that can escape to space, and surface temperatures will continue to rise.

This exceptional year of extreme weather shows how dangerous life has already become with 1.3ยฐC of human-induced warming, and highlights the urgency of moving away from planet-heating fossil fuels. The science is clear: the complex link between global warming and extreme events is driven by the physics of our climate system, and the connection grows stronger with every fraction of a degree of warming.

What do you think? Given that developing countries often lack the historical climate data needed to fully understand local impacts yet face the greatest risks from extreme weather, how can the global community address this disparity while accelerating climate action?

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References
  1. https://www.epa.gov/climatechange-science/basics-climate-change
  2. https://wmo.int/news/media-centre/wmo-report-documents-spiralling-weather-and-climate-impacts
  3. https://royalsociety.org/news-resources/projects/climate-change-evidence-causes/basics-of-climate-change/
  4. https://www.noaa.gov/jetstream/atmosphere/energy
  5. https://science.nasa.gov/climate-change/faq/what-is-the-greenhouse-effect/
  6. https://www.ces.fau.edu/nasa/module-2/how-greenhouse-effect-works.php
  7. https://bio.libretexts.org/Courses/Gettysburg_College/01:_Ecology_for_All/02:_The_Physical_Environment/2.05:_Earth's_Energy_Balance
  8. https://earthobservatory.nasa.gov/features/EnergyBalance/page6.php
  9. https://energyeducation.ca/encyclopedia/The_greenhouse_effect_and_Earth's_energy_budget
  10. https://scied.ucar.edu/learning-zone/climate-change-impacts/water-cycle-climate-change
  11. https://news.climate.columbia.edu/2019/09/23/climate-change-impacts-water/
  12. https://www.mhwm.pl/Acceleration-of-the-hydrological-cycle-and-its-impact-on-water-availability-over,188920,0,2.html
  13. https://www.un.org/depts/los/global_reporting/WOA_RPROC/Chapter_04.pdf
  14. https://www.metlink.org/resource/the-changing-water-cycle/
  15. https://www.worldweatherattribution.org/when-risks-become-reality-extreme-weather-in-2024/
  16. https://earth.org/extreme-weather-events-in-2024-led-to-highest-number-of-new-displacements-since-2008/
  17. https://www.climate.gov/news-features/blogs/beyond-data/2024-active-year-us-billion-dollar-weather-and-climate-disasters
  18. https://www.climatecentral.org/climate-matters/2024-in-review
  19. https://yaleclimateconnections.org/2024/10/climate-change-made-hurricane-helene-and-other-2024-disasters-more-damaging-scientists-find/
  20. https://wmo.int/media/magazine-article/observing-climate-challenges-21st-century
  21. https://esg.sustainability-directory.com/question/what-are-the-key-challenges-in-climate-data/
  22. https://frontiersin.org/articles/10.3389/fclim.2021.787519/full
  23. https://www.worldweatherattribution.org/climate-change-fuelled-extreme-weather-in-2023-expect-more-records-in-2024/

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Introduction to Climate Change

1 Atmospheric Structure and Composition

  1. Weather and Climate
  2. Climate – Global, Regional and Local
  3. The Atmosphere
  4. Structure of the Atmosphere
  5. Climate Change and Climate Variability

2 Solar Radiation and Global Energy Budget

  1. Solar Radiation
  2. The Greenhouse Effect
  3. Greenhouse Gases
  4. Global Warming Potential
  5. Trends in Greenhouse Gases Emissions

3 Radiative Forcing

  1. Natural Driversโ€™ of Climate Change
  2. Anthropogenic Driversโ€™ of Climate Change
  3. What is Radiative Forcing?

4 Climate Feedbacks

  1. What is a Climate Feedback?
  2. Water Vapour Feedback
  3. Snow and Ice Albedo Feedback
  4. Cloud Feedbacks
  5. Lapse-Rate Feedback
  6. Ocean-circulation Feedback

5 Account of Past Climate

  1. Palaeoclimate
  2. Glimpse of Earthโ€™s Climate through Ages
  3. Sources of Palaeoclimatic Data
  4. Climate of the Quaternary Period

6 Environmental Indicators and Instrumental Records

  1. Factors affecting the Earthโ€™s Climate System
  2. The Measurement of Climate Change
  3. Annual Resolution Data from Proxy Record
  4. Centennial to Millennial Scale Data from Proxy Records

7 Human Footprints on Global Warming

  1. Human Population Growth
  2. Human Population Growth
  3. Industrialization
  4. Deforestation
  5. Direct and Indirect Impacts of Deforestation
  6. Urbanization
  7. Particulates
  8. Desertification
  9. Stratospheric Ozone Depletion

8 Predicting Future Climates

  1. Analogues from Past Climate
  2. Climate Models
  3. Types of Climate Models
  4. Greenhouse Gas Emission Scenarios
  5. Time Dependent Models
  6. Representative Concentration Pathways (RCPs)

9 Temperature Regime

  1. Introduction
  2. Trends in Temperature
  3. Trends in Precipitation
  4. Trends in Rise in Sea Level
  5. Global Warming and Cyclones
  6. Let Us Sum Up
  7. Keywords

10 Precipitation Regime

  1. The Hydrological Cycle
  2. Monsoon
  3. Global Monsoon System
  4. Climates: Global, Regional and Local
  5. El Niรฑo
  6. Weather Aberrations
  7. Climate Uncertainties
  8. Future Climate in the 21st Century

11 Composition Regime

  1. Impact of Climate Change on Biodiversity
  2. Snow Line
  3. Timberline
  4. Permafrost
  5. Methane Clathrates
  6. Forest Fires
  7. Aerosols and Climate Interactions

12 Extreme Climate Events

  1. Introduction
  2. Extreme Events
  3. Relationship Between Climate Change and Extreme Events
  4. Occurrence of Extreme Events – Sea Level Rise
  5. Occurrence of Extreme Events – Melting of Glaciers and Ice Caps
  6. Occurrence of Extreme Events – Drought
  7. Occurrence of Extreme Events – Forest Fires
  8. Occurrence of Extreme Events – Floods
  9. Occurrence of Extreme Events – Cyclones

13 International Initiatives

  1. History of Climate Change Debate
  2. Rio Declaration on Environment and Development
  3. UNFCCC
  4. IPCC
  5. Climate Change and the North-South Debate
  6. Kyoto Protocol
  7. Marrakesh Accord
  8. Bali Action Plan
  9. Copenhagen Summit
  10. Paris Agreement on Climate Change
  11. India’s Response Framework

14 National Level Action Plan

  1. Copenhagen Summit 2009
  2. India and Copenhagen Summit
  3. India’s Policy and Action towards Renewable Energy Sources
  4. Paris Agreement
  5. National Action Plan on Climate Change

15 State Level Action Plan

  1. Introduction
  2. Policy Formulation
  3. Agencies involved in Policy Formulation in India
  4. State Governments’ Efforts to Address Climate Change: State Action Plan
  5. Tamil Nadu
  6. Delhi
  7. Jharkhand
  8. Assessment of State Action Plans on Climate Change

16 Local Level Initiatives

  1. Status of Degradation of Natural Resources
  2. Techniques of Natural Resources Management
  3. Case Studies on Natural Resources Management
  4. Climate Change and Socio-Economic Vulnerability to Cyclones and Floods in Coastal Odisha โ€“ A Case Study of Women Self Help Group