Understanding the causes and multifaceted impacts of climate change is crucial for appreciating the urgency of the problem and for formulating effective responses. The current rapid warming trend is overwhelmingly attributed to human activities.
A. Causes of Climate Change
I. Natural Causes (Climate Variability)
These factors influence climate over geological timescales but don't explain current rapid warming.
Variations in Solar Output
Sun's energy output varies (e.g., ~11-year solar cycle). Satellite data since 1970s show no net increase to explain current warming. Recent solar activity has been low while temperatures rise.
Milankovitch Cycles
Long-term orbital changes driving past ice ages. Operates on too long timescales (10,000s-100,000s years) for current warming.
- Eccentricity: Orbit shape (~100,000 yrs)
- Obliquity: Axial tilt (~41,000 yrs)
- Precession: Axis wobble (~26,000 yrs)
Volcanic Eruptions
Large eruptions inject SO₂ (sulfate aerosols) causing short-term cooling (1-3 yrs, e.g., Mt. Pinatubo ~0.5°C). CO₂ release is minimal compared to human emissions.
Plate Tectonics
Continental drift over millions of years, affecting ocean currents and long-term climate patterns. Geological timescales.
Ocean Variability
Natural fluctuations like ENSO (El Niño) and PDO cause short-term (years-decades) regional/global variations, but not the long-term warming trend.
II. Anthropogenic (Human-Caused) Causes
The dominant drivers of current rapid climate change, primarily through the enhanced greenhouse effect.
Increased Greenhouse Gases (GHGs)
Primary driver of current global warming.
For electricity, transport, industry, heating/cooling. Releases vast CO₂ (most significant), CH₄, N₂O.
Reduces CO₂ absorption (loss of carbon sinks). Burning/decomposition releases stored CO₂. Alters soil carbon & albedo.
CH₄ (Methane): Livestock digestion, manure, rice cultivation.
N₂O (Nitrous Oxide): Nitrogen fertilizers, manure management.
F-gases (HFCs, PFCs, SF₆, NF₃): Potent GHGs from refrigerants, solvents, etc.
CO₂: Cement production (calcination).
Other CH₄ & N₂O emissions.
CH₄: Landfill decomposition.
CH₄ & N₂O: Wastewater treatment.
CO₂: Waste incineration.
Aerosols (Particulate Matter)
Complex effects:
- Cooling Effect (most aerosols, e.g., sulfates): Reflect solar radiation, modify clouds. Partially offsets GHG warming.
- Warming Effect (e.g., black carbon/soot): Absorbs solar radiation, reduces snow/ice albedo.
Overall net effect estimated as cooling (with uncertainty). Reducing aerosol pollution could unmask more GHG warming.
Changes in Land Surface Albedo
Albedo = surface reflectivity. Lighter surfaces (snow, ice) = high albedo; darker (forests, oceans) = low albedo. Deforestation, urbanization, melting ice alter albedo and energy balance.
B. Impacts of Climate Change
Impacts are observed globally, interconnected, and projected to intensify. They can create cascading effects.
I. Physical Impacts
Rising Global Temperatures
Increased average land/ocean temperatures.
More frequent, intense, longer heatwaves (health, agriculture, ecosystem risks).
Changes in temperature extremes.
Changes in Precipitation
Increased variability: intense rainfall/floods in some regions, severe droughts in others.
Shifts in seasonal patterns affecting water availability.
Melting Ice and Snow (Cryosphere)
Sea Level Rise
Caused by thermal expansion & melting land ice.
Impacts: Coastal inundation/erosion, flooding, salinization, displacement, infrastructure damage. SIDS vulnerable.
Ocean Acidification
Oceans absorb CO₂, forming carbonic acid, lowering pH.
Hinders shell/skeleton formation in marine calcifiers (corals, shellfish). Disrupts food webs.
Extreme Weather Events
More frequent/intense heatwaves, heavy precipitation/floods, droughts, intense tropical cyclones, wildfires.
II. Impacts on Ecosystems & Biodiversity
Species Range & Phenology Shifts
Habitat Degradation & Loss
Increased Extinction Risk
Spread of Pests & Diseases
III. Impacts on Human Systems
Human Health
Agriculture & Food Security
Water Resources
Infrastructure & Settlements
Economic Impacts
Social Impacts
Differential Impacts
Impacts are not uniform. Developing countries, SIDS, Arctic regions, and marginalized communities are often most vulnerable due to location, dependence on climate-sensitive sectors, and limited adaptive capacity.
Feedback Loops
Positive Feedbacks (Amplify Warming)
Examples: Ice-Albedo, Permafrost Thaw, Water Vapor, Forest Dieback.
Negative Feedbacks (Dampen Warming)
Examples: Carbon Fertilization (limited by nutrients/water), Chemical Weathering (very long timescales).
Illustrative GHG Contributions (Conceptual)
Note: Proportions are illustrative.
UPSC Exam Relevance
Prelims Focus
- Natural vs. Anthropogenic causes.
- Major GHG sources, Global Warming Potential (GWP).
- Impacts: Coral bleaching, ocean acidification, sea-level rise, permafrost thaw.
- Concepts: Albedo, Milankovitch cycles, ENSO.
- Feedback loops.
Mains Focus (GS-I, GS-III)
- Anthropogenic causes & diverse impacts on India.
- Ocean acidification: phenomenon & consequences.
- Impacts on Indian agriculture & water resources; adaptation strategies.
- Climate change as a developmental & security challenge.
- Linkages to disaster management (extreme weather).
Related Previous Year Questions (PYQs) Insights
- Factors for 'water stress' (climate change exacerbates).
- Importance of 'Blue Carbon' initiative.
- 'Climate Neutral Now' initiative.
- Questions on GHGs, sources, GWP, specific impacts.
- "Climate Change is a global problem. How India will be affected...?" (UPSC Mains 2017)
- Causes of mangrove depletion (sea-level rise relevant).
- Consequences of 'Dead Zones' (warming exacerbates).
- Causes/effects of landslides (climate change can increase risk).