🗞️ Why in News A study published in AGU Advances (American Geophysical Union) found that the Amazon rainforest became a net carbon source during the severe 2023 El Niño drought, releasing between 10 and 170 million tonnes of CO₂ during September–November 2023. This reversal of the world’s largest terrestrial carbon sink has profound implications for global climate targets and raises urgent questions about irreversible tipping points.
The Study — Key Findings
- Journal: AGU Advances (published early 2026)
- Lead author: Saulo Botía (Max Planck Institute for Biogeochemistry, Germany)
- Period studied: September–November 2023 (peak of El Niño drought)
- Method: Atmospheric CO₂ concentration measurements from monitoring stations across the Amazon basin, combined with inverse modelling
- Finding: The Amazon released 10–170 million tonnes of CO₂ — a net carbon source instead of a sink
- Cause: Extreme drought reduced photosynthesis (trees absorb less CO₂ when water-stressed) while simultaneously increasing tree mortality, wildfires, and decomposition
- Context: The 2023 drought was the most severe on record in the Amazon — river levels fell to historic lows, temperatures exceeded 40°C in parts of the basin
Why the Amazon Matters — Global Carbon Cycle
- The Amazon is the world’s largest tropical rainforest — ~6.7 million km² across 9 countries (Brazil: ~60%)
- Contains an estimated 390 billion individual trees of ~16,000 species
- Historically absorbed ~2 billion tonnes of CO₂ per year — acting as a massive carbon sink
- This absorption capacity has been declining steadily — now estimated at ~1.2 billion tonnes/year (a 40% reduction)
- The Amazon stores 150–200 billion tonnes of carbon in its biomass — releasing even a fraction would be catastrophic
- “Flying rivers”: The Amazon generates ~20 billion tonnes of water vapour daily through transpiration — this moisture cycle drives rainfall patterns across South America and influences global atmospheric circulation
The 2023 El Niño — What Happened
- The 2023 El Niño was among the strongest on record — global mean temperature breached 1.5°C above pre-industrial levels for the first time (calendar year)
- El Niño brought severe drought to the Amazon basin — reduced rainfall, extreme heat, record-low river levels
- Rio Negro (major Amazon tributary) fell to its lowest level in over 120 years of records
- Massive wildfires swept through the Amazon and Cerrado biome — Brazil recorded its worst fire season
- Aquatic ecosystem collapse: River dolphins, fish, and turtles died in mass mortality events as water temperatures soared
⊕ Additional UPSC Concepts (Supplementary Material)
The following sections provide supplementary explanatory material beyond the article — covering key concepts that UPSC aspirants must understand in this context.
El Niño and La Niña — The ENSO Cycle
What is ENSO?
- ENSO = El Niño–Southern Oscillation — a periodic climate pattern in the tropical Pacific Ocean
- It is the most important driver of year-to-year climate variability globally
- ENSO has three phases: El Niño (warm), La Niña (cool), and Neutral
El Niño
- Definition: Abnormal warming of sea surface temperatures (SSTs) in the central and eastern equatorial Pacific Ocean (Niño 3.4 region: 5°N–5°S, 120°W–170°W)
- Threshold: SST anomaly ≥ +0.5°C sustained for 5 consecutive overlapping 3-month periods
- Mechanism:
- Normally, trade winds blow east-to-west across the Pacific, pushing warm surface water toward Indonesia/Australia
- This causes cold water upwelling off the coast of South America (Peru/Ecuador)
- During El Niño, trade winds weaken or reverse → warm water spreads eastward → upwelling diminishes
- Global impacts:
- India: Weaker monsoon (reduced rainfall) — historically, El Niño years correlate with below-normal monsoon in India (not always — 2023 monsoon was near-normal despite El Niño)
- Amazon/Australia: Drought, wildfires, reduced rainfall
- South America (west coast): Heavy rains, floods in Peru/Ecuador
- Global temperature: El Niño years tend to be warmer globally (2023 was the hottest year on record)
- Marine life: Collapse of fisheries off Peru (reduced upwelling = reduced nutrients)
La Niña
- Definition: Abnormal cooling of SSTs in the central and eastern equatorial Pacific
- Threshold: SST anomaly ≤ -0.5°C sustained for 5 consecutive overlapping 3-month periods
- Mechanism: Trade winds strengthen → more warm water pushed westward → stronger cold upwelling off South America
- Global impacts:
- India: Generally above-normal monsoon rainfall — La Niña years are often good for Indian agriculture
- Amazon/Southeast Asia/Australia: Above-normal rainfall, floods
- Global temperature: La Niña years tend to be cooler globally
- Atlantic hurricanes: La Niña reduces wind shear over the Atlantic → more intense hurricane seasons
Indian Ocean Dipole (IOD) — Complementary Concept
- IOD = difference in SSTs between the western Indian Ocean (Arabian Sea) and eastern Indian Ocean (off Sumatra)
- Positive IOD: Warmer western Indian Ocean → enhances Indian monsoon (can counteract El Niño’s negative effect)
- Negative IOD: Warmer eastern Indian Ocean → weakens Indian monsoon
- 2023 example: Positive IOD partly offset El Niño’s impact, helping India receive near-normal monsoon despite strong El Niño
Amazon Tipping Point — The Savannification Thesis
What is a Tipping Point?
- A tipping point is a threshold beyond which a system undergoes irreversible, self-reinforcing change — even if the original pressure is removed
- In climate science, tipping points represent non-linear, abrupt shifts in Earth systems
The Amazon Tipping Point
- Scientists estimate that if 20–25% of the Amazon is deforested, the forest may cross a tipping point and begin converting to savanna or degraded grassland — a process called savannification
- Current deforestation: ~17% of the original Amazon has been cleared (mostly in the “arc of deforestation” in southern/eastern Brazil)
- The tipping point is driven by a feedback loop:
- Deforestation reduces transpiration → less moisture recycled into the atmosphere
- Less moisture → reduced rainfall → remaining forest dries out
- Dry forest becomes vulnerable to fire → more trees die → more deforestation
- The cycle accelerates — the forest can no longer sustain itself
- A 4°C global temperature rise could trigger widespread savannification regardless of deforestation levels
- Timeline: Some models suggest parts of the eastern Amazon could cross the tipping point by 2050 under current trajectories
Other Major Tipping Points (for UPSC)
| Tipping Element | Threshold | Consequence |
|---|---|---|
| Greenland Ice Sheet | ~1.5°C global warming | 7m sea level rise over centuries |
| West Antarctic Ice Sheet | ~1.5–2°C | 3.3m sea level rise |
| Amazon Rainforest | 20–25% deforestation or ~4°C | Savannification, massive carbon release |
| Atlantic Meridional Overturning Circulation (AMOC) | Freshwater influx from ice melt | Disruption of Gulf Stream, European cooling |
| Permafrost | ~2°C | Methane release, accelerated warming |
| Coral Reefs | 1.5–2°C | Mass bleaching, ecosystem collapse |
Planetary Boundaries Framework
- Developed by Johan Rockström (Stockholm Resilience Centre) in 2009
- Identifies 9 planetary boundaries — safe operating limits for human civilisation
- As of 2023–24, 7 of 9 boundaries have been breached:
| Boundary | Status |
|---|---|
| Climate change | Breached |
| Biosphere integrity (biodiversity) | Breached |
| Land-system change | Breached |
| Biogeochemical flows (N & P) | Breached |
| Freshwater change | Breached |
| Novel entities (chemical pollution) | Breached |
| Atmospheric aerosol loading | Breached |
| Ocean acidification | At risk |
| Stratospheric ozone depletion | Within safe limits |
- The Amazon drought-to-source reversal is a manifestation of multiple boundaries being crossed simultaneously — climate change + biosphere integrity + land-system change
Carbon Sink vs Carbon Source — Key Distinction
- Carbon sink: Any system that absorbs more CO₂ than it releases (forests, oceans, soils, peatlands)
- Carbon source: Any system that releases more CO₂ than it absorbs
- Global carbon sinks: Oceans absorb ~25% of annual CO₂ emissions; land ecosystems (primarily forests) absorb ~30%
- The danger: If major sinks flip to sources, atmospheric CO₂ accumulation accelerates — a positive feedback loop that makes climate targets (1.5°C/2°C) even harder to achieve
- Amazon’s shift: The 2023 reversal may not be permanent — but if droughts become more frequent (as climate models predict), the Amazon could become a persistent net source within decades
Critical Evaluation for UPSC Mains
Why This Matters
- Paris Agreement targets: If the Amazon permanently flips from sink to source, the global carbon budget for 1.5°C is effectively exhausted
- India’s vulnerability: El Niño-driven Amazon droughts correlate with weaker Indian monsoons — the same climate pattern that threatens both systems
- Biodiversity loss: Amazon holds 10% of all species on Earth — savannification would trigger mass extinction
- Transboundary governance: The Amazon spans 9 countries — no single nation controls its fate; parallels with India’s transboundary river/forest governance challenges
- SDG interconnections: SDG 13 (Climate Action), SDG 15 (Life on Land), SDG 6 (Clean Water) are all implicated
India-Specific Connections
- India’s forests are also under stress — Forest Survey of India reports increasing fire frequency in central Indian forests
- India’s carbon sink target under NDC: additional 2.5–3 billion tonnes CO₂ equivalent through forest/tree cover by 2030
- Compensatory Afforestation Fund (CAMPA): ₹50,000+ crore accumulated but utilisation remains low
- India’s Western Ghats — a biodiversity hotspot — faces similar deforestation-rainfall feedback risks (Gadgil Report warned of this)
UPSC Angle
- Prelims: ENSO (El Niño, La Niña), IOD, AGU, carbon sink vs source, planetary boundaries, tipping points, Amazon basin countries, savannification, AMOC, Paris Agreement carbon budget, NDC
- Mains GS-1: Geography — ENSO cycle and its global impacts, Indian monsoon variability, El Niño–La Niña mechanism, IOD, tropical rainforest climate
- Mains GS-3: Environment — carbon cycle, forest as carbon sinks, tipping points, climate change impacts, biodiversity loss, Paris Agreement, India’s NDC targets, CAMPA
- Essay: “When the lungs of the Earth exhale carbon, no nation can hold its breath”
📌 Facts Corner — Knowledgepedia
Amazon 2023 Drought Study:
- Journal: AGU Advances; Lead author: Saulo Botía (Max Planck Institute)
- Amazon released 10–170 million tonnes CO₂ (Sep–Nov 2023)
- Cause: El Niño-driven drought — worst on record in Amazon
- Rio Negro fell to lowest level in 120+ years
- 2023 was hottest year on record globally (1.5°C breached for first time)
Amazon Rainforest:
- Area: ~6.7 million km² across 9 countries (Brazil ~60%)
- Trees: ~390 billion individuals, ~16,000 species
- Historical carbon absorption: ~2 billion tonnes CO₂/year (now ~1.2 billion)
- Carbon stored in biomass: 150–200 billion tonnes
- Transpiration: ~20 billion tonnes water vapour/day (“flying rivers”)
- 10% of all species on Earth found in Amazon
El Niño–Southern Oscillation (ENSO):
- El Niño: warming of central/eastern equatorial Pacific SSTs (≥ +0.5°C anomaly)
- La Niña: cooling of central/eastern equatorial Pacific SSTs (≤ -0.5°C anomaly)
- El Niño → weaker Indian monsoon (generally); La Niña → stronger monsoon
- IOD (Indian Ocean Dipole): positive IOD can offset El Niño’s negative impact on Indian monsoon
- Niño 3.4 region: 5°N–5°S, 120°W–170°W (key monitoring zone)
Tipping Points:
- Amazon tipping point: 20–25% deforestation → savannification
- Current Amazon deforestation: ~17% of original forest cleared
- 4°C warming could trigger savannification regardless of deforestation
- Greenland Ice Sheet: ~1.5°C → 7m sea level rise
- AMOC disruption: freshwater from ice melt → Gulf Stream weakening
- Permafrost: ~2°C → methane release acceleration
Planetary Boundaries:
- Framework: Johan Rockström, Stockholm Resilience Centre (2009)
- 9 boundaries identified; 7 of 9 breached (as of 2023–24)
- Only ozone depletion within safe limits; ocean acidification at risk
India Connections:
- India’s NDC carbon sink target: additional 2.5–3 billion tonnes CO₂ eq. by 2030
- CAMPA fund: ₹50,000+ crore accumulated (low utilisation)
- India’s forest cover: 21.76% of geographic area (FSI 2023)
- Western Ghats: similar deforestation-rainfall feedback risk
Other Relevant Facts:
- Paris Agreement (2015): limit warming to 1.5°C/2°C above pre-industrial
- Global carbon budget for 1.5°C: ~250 billion tonnes CO₂ remaining (IPCC AR6)
- Oceans absorb ~25% of annual CO₂; land ecosystems ~30%
- Amazon fires 2023: worst fire season in Brazil in decades
- Cerrado biome: tropical savanna adjacent to Amazon — also heavily deforested
- IPCC AR6 (2021–23): Sixth Assessment Report — warned of tipping point cascades
Sources: Down to Earth, AGU Advances, IPCC AR6, Stockholm Resilience Centre, NASA Earth Observatory