Forests are among Earth’s most powerful allies in the fight against climate change. They act as natural carbon storage systems, absorbing carbon dioxide from the atmosphere and holding it in their trunks, branches, leaves, roots, and soil. When these forests are cleared or burned, that stored carbon is released back into the atmosphere. The scale of this problem is staggering. In 2023 alone, global tropical forest loss totaled 3.7 million hectares, releasing carbon equivalent to roughly six percent of global emissions that year.

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How forests function as carbon sinks

Forest ecosystems serve vital functions in maintaining Earth’s carbon cycle. Trees and plants absorb atmospheric carbon dioxide through photosynthesis, converting it into carbon that becomes part of their physical structure. Forests remove an estimated 16 billion tonnes of carbon dioxide from the atmosphere annually, which equals about half of the annual emissions from burning fossil fuels. Tropical rainforests are particularly effective at this process, sequestering more carbon dioxide than boreal and temperate forests combined.

However, this carbon removal is partially offset by emissions from forest loss. When trees are cut down through logging or destroyed by wildfires, they release stored carbon. Emissions from tree cover loss averaged 8.1 billion tonnes annually over the past 20 years. The net effect is that forests still remove approximately 7.6 billion tonnes of carbon dioxide each year, but this benefit is under constant threat from ongoing deforestation.

What deforestation means and how it happens

Deforestation refers to the deliberate conversion of forests to non-forested land uses. This includes clearing land for agriculture, urban development, logging operations, or other purposes. According to the Food and Agriculture Organization, deforestation is defined as the conversion of forest to another land use or the long-term reduction of tree canopy cover below a ten percent threshold.

The scale of forest loss is alarming. Projections suggest that forest area in developing regions could decrease by 200 to 490 million hectares between 2000 and 2050. This massive reduction would severely diminish water retention capacity and accelerate soil erosion, with particularly severe impacts in lowland areas that are already prone to flooding.

Primary drivers of forest destruction

The main cause of deforestation is agricultural expansion. Agriculture is responsible for at least 80 percent of tropical deforestation, with approximately 60 percent of all tropical deforestation driven by farming land expansion. Other significant causes include shifting agriculture practices, urbanization, infrastructure development, timber plantations, logging operations, fuel wood collection, overgrazing, human-induced forest fires, and mining activities.

Many of these activities create a destructive cycle. Rainforest soils are often nutrient-poor, with most nutrients locked in the forest vegetation itself. When forests are cleared and burned, the nutrients from ash are quickly depleted, forcing farmers to move on to clear new areas. This pattern of clearing, planting, depleting, and repeating drives continuous forest loss.

The connection between deforestation and global warming

As of 2019, deforestation is responsible for about 11 percent of global greenhouse gas emissions. This contribution to climate change happens through multiple pathways. First, when forests are cleared, we lose a crucial carbon sink that would otherwise continue absorbing atmospheric carbon dioxide. Second, the act of cutting down trees releases the carbon they had been storing. Third, what happens to the felled trees matters tremendously. Whether left to decompose on the forest floor or burned, they release additional emissions into the atmosphere.

The replacement land use often compounds the problem. When deforested land becomes pasture or cropland, these new uses generate their own greenhouse gas emissions, including methane from livestock and nitrous oxide from fertilizers. Combined, these three factors mean that deforestation and the agriculture that replaces forests account for roughly a quarter of all global emissions.

Deforestation rates vary significantly by region. Some tropical areas have become net sources of carbon emissions, meaning they release more carbon dioxide than their remaining forests can absorb. Southeast Asian tropical rainforests fall into this category. Meanwhile, the Amazon and Congo Basin rainforests still function as net carbon sinks, though their capacity is diminishing as forest loss continues.

The world loses 10 million hectares of forests annually, with much of this devastation concentrated in tropical and subtropical regions. This ongoing loss threatens global climate stability and makes achieving international climate targets increasingly difficult.

Forest degradation beyond clear-cutting

Not all forest damage involves complete removal of trees. Forest degradation reduces forest quality and biomass through unsustainable harvest practices, selective logging, fires, and excessive fuelwood collection. These activities diminish the forest’s capacity to store carbon and provide ecosystem services, even when the forest technically remains standing.

Degraded forests lose their ability to regulate local climate effectively. Trees release moisture that cools surrounding air, and when this process is disrupted through degradation or deforestation, local temperatures can rise. Research shows that tree removal can increase local air temperatures and daily temperature variation, affecting both human communities and wildlife.

Forests support biodiversity and livelihoods

Beyond their climate role, forests are biodiversity hotspots. Forests are home to about 80 percent of the world’s terrestrial biodiversity, providing habitat for countless plant and animal species. Many of these species exist nowhere else on Earth, making their survival entirely dependent on forest preservation.

Human communities also depend heavily on forests. Approximately 1.6 billion people rely on forests for all or part of their livelihoods, using forest resources for food, shelter, energy, medicine, and income. Among these, about one billion are among the world’s poorest populations. When forests disappear, these communities lose not just natural resources but their entire way of life and economic foundation.

The path forward

Halting deforestation could reduce emissions by 4 gigatonnes annually, representing a significant contribution to climate change mitigation. Protecting existing forests, combined with reforestation and afforestation efforts, can increase carbon sequestration while reducing emissions from forest loss. However, success requires addressing the underlying economic drivers of deforestation, particularly agricultural expansion.

Solutions must balance conservation goals with the needs of local communities and food security demands. This includes implementing sustainable forest management practices, supporting forest-dependent communities in developing alternative livelihoods, and transforming agricultural systems to increase productivity on existing farmland rather than expanding into forested areas. Only through such integrated approaches can we preserve forests while meeting human needs.

What do you think? How can societies balance the need for agricultural land with forest conservation? What role should developed nations play in supporting forest protection in developing countries where most deforestation occurs?

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References
  1. https://www.climatecouncil.org.au/deforestation/
  2. https://blogs.worldbank.org/en/opendata/deforestation-accelerating-climate-change-and-threatening-biodiversity
  3. https://www.rainforest-alliance.org/insights/what-is-the-relationship-between-deforestation-and-climate-change/
  4. https://en.wikipedia.org/wiki/Deforestation_and_climate_change
  5. https://www.unep.org/news-and-stories/story/how-halting-deforestation-can-help-counter-climate-crisis
  6. https://www.genevaenvironmentnetwork.org/resources/updates/importance-of-forests-and-the-role-of-geneva/
  7. https://iucn.org/resources/issues-brief/deforestation-and-forest-degradation

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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