Climate change science, IPCC & India's NDCs
Climate change science fundamentals, the IPCC's assessment architecture, the UNFCCC-Paris framework, and India's updated NDCs and net-zero pledge for UPSC.
The radiative basis of climate change
Climate change science rests on a measurable physical mechanism: greenhouse gases (GHGs)—carbon dioxide (CO2), methane (CH4), nitrous oxide (N2O), and fluorinated gases—absorb outgoing longwave (infrared) radiation and re-emit it, warming the lower atmosphere. This is the enhanced greenhouse effect, distinct from the natural greenhouse effect that keeps Earth habitable. Svante Arrhenius first quantified the CO2-temperature link in 1896; the Keeling Curve, begun at Mauna Loa in 1958, provided the empirical record of rising atmospheric CO2, which crossed 420 ppm in 2023 against a pre-industrial baseline of about 280 ppm.
Key metrics and concepts
Gases differ in warming potency. Global Warming Potential (GWP) indexes a gas against CO2 over a horizon (usually 100 years): methane's GWP-100 is roughly 28–34, nitrous oxide about 265–298, and sulphur hexafluoride over 23,000. Radiative forcing, measured in W/m2, expresses the net change in energy balance; CO2 contributes the largest positive forcing. Carbon sinks—oceans and terrestrial vegetation—absorb roughly half of anthropogenic emissions, while the residual stays airborne, giving CO2 an effective atmospheric lifetime of centuries.
The IPCC's Sixth Assessment Report (AR6, Working Group I, 2021) concluded it is unequivocal that human influence has warmed the climate, with global surface temperature about 1.1°C above 1850–1900 levels. The carbon budget concept is exam-critical: to keep warming below 1.5°C with 50% probability, AR6 estimated a remaining budget of roughly 500 GtCO2 from 2020. Feedback loops amplify warming—ice-albedo feedback (melting ice exposes dark surfaces), permafrost methane release, and water-vapour feedback.
Impacts of relevance to India
India is acutely exposed. The IPCC and the Ministry of Earth Sciences' 2020 assessment Climate Change Over the Indian Region document accelerating sea-level rise along the 7,500-km coastline, intensifying heatwaves, erratic monsoons, glacial retreat in the Hindu Kush Himalaya, and increased cyclone intensity in the Arabian Sea. Distinguish mitigation (reducing emissions/enhancing sinks) from adaptation (adjusting to impacts)—a recurring Prelims-Mains hinge. Note also climate justice and Common But Differentiated Responsibilities (CBDR-RC), the equity principle India consistently invokes, grounded in Article 3.1 of the 1992 UNFCCC.
Understanding the science prevents factual errors that examiners exploit: confusing ozone depletion (a stratospheric chemistry problem governed by the 1987 Montreal Protocol) with global warming, or conflating weather with climate. The 2016 Kigali Amendment to the Montreal Protocol, which India ratified in 2021, links the two regimes by phasing down hydrofluorocarbons (HFCs)—potent GHGs introduced as ozone-friendly substitutes.