๐ก๏ธ Chapter 06 ยท Topic 02 ยท Climate Change
Effects of Climate Change
Sea level rise, glacial retreat, extreme weather events, coral bleaching, ocean acidification, species extinction, food security, and India-specific impacts โ complete UPSC & PSC notes.
๐ Sea Level Rise
Sea level rise is one of the most significant and well-documented effects of climate change. It occurs due to two main processes:
- Thermal expansion โ as ocean water warms, it expands in volume (accounts for ~50% of observed rise)
- Glacial and ice sheet melt โ melting of mountain glaciers, Greenland Ice Sheet, and Antarctic Ice Sheet adds water to oceans
- Current rate: approximately 3.3โ3.7 mm per year (accelerating; was ~1.4 mm/year in the 20th century)
- Total rise since 1900: approximately 20 cm
- Projected rise by 2100: 0.3โ1.0 m under various scenarios (could be higher if ice sheets destabilise)
โญ Countries Most at Risk: Maldives (average elevation ~1.5 m โ could be uninhabitable by 2100), Tuvalu (Pacific island nation โ already signing agreements for relocation), Bangladesh (17% of land area could be submerged; 20 million people displaced), Kiribati, Marshall Islands. India’s coastal cities at risk: Mumbai, Chennai, Kolkata, Kochi, Visakhapatnam.
India’s Coastal Vulnerability
- India has a coastline of 7,516 km with 9 coastal states and 4 union territories
- Over 170 million people live in India’s coastal districts
- Sundarbans (West Bengal) โ world’s largest mangrove delta; several islands already submerged; Lohachara Island was the first inhabited island to be submerged (2006)
- Mumbai: Bandra-Kurla Complex, Nariman Point, and low-lying areas at risk
- Chennai: Marina Beach area and northern coastal zones vulnerable
- Kolkata: built on the Gangetic delta โ highly vulnerable to flooding and sea level rise
๐๏ธ Glacial Retreat
- Glaciers worldwide are retreating at accelerating rates due to rising temperatures
- Himalayan glaciers โ called the “Third Pole” โ contain the largest concentration of ice outside the polar regions
- Over 9,000 glaciers in the Himalayas; feed major rivers: Ganga, Indus, Brahmaputra, Yangtze, Mekong
- Gangotri Glacier (source of Ganga) โ retreating at ~22 metres per year; has retreated ~2 km since 1780
- Siachen Glacier โ world’s largest non-polar glacier; also retreating
- Short-term effect: increased river flow (glacial melt adds water) โ flooding
- Long-term effect: glaciers disappear โ rivers lose their dry-season flow โ water scarcity for hundreds of millions
๐ GLOF (Glacial Lake Outburst Flood): As glaciers melt, they form glacial lakes dammed by ice or moraine. When these dams fail, catastrophic floods occur downstream. India has experienced several GLOFs โ the 2021 Chamoli disaster (Uttarakhand) was linked to a glacial lake outburst, killing 200+ people. GLOFs are increasing with climate change.
๐ช๏ธ Extreme Weather Events
Climate change is making extreme weather events more frequent, more intense, and longer-lasting.
| Event Type | Climate Change Link | India Examples |
|---|---|---|
| Cyclones | Warmer oceans provide more energy; rapid intensification more common; slower movement = more rainfall | Cyclone Amphan (2020), Cyclone Biparjoy (2023), increasing Bay of Bengal cyclone intensity |
| Floods | Warmer atmosphere holds more moisture (7% more per 1ยฐC) โ heavier rainfall events | Kerala floods (2018, 2019), Uttarakhand floods (2013, 2021), Chennai floods (2015) |
| Droughts | Altered precipitation patterns; increased evaporation; shifting monsoon | Maharashtra drought (2018โ19), Bundelkhand chronic drought |
| Heatwaves | Baseline temperatures higher; heat extremes more frequent and intense | India heatwaves (2022, 2023) โ temperatures exceeding 45ยฐC in Rajasthan, UP, Delhi |
| Wildfires | Hotter, drier conditions; longer fire seasons | Uttarakhand forest fires (increasing frequency) |
| Cold waves | Arctic warming disrupts polar vortex โ cold air spills south | North India cold waves; paradoxically linked to Arctic warming |
โญ Attribution Science: Scientists can now calculate how much more likely a specific extreme event was due to climate change. For example, the 2022 Pakistan floods were made 50% more likely by climate change. The 2021 North American heat dome was “virtually impossible” without climate change. This field is called extreme event attribution.
๐ชธ Coral Bleaching
- Corals live in a symbiotic relationship with zooxanthellae (photosynthetic algae) that live in their tissues and provide 90% of their energy
- When water temperature rises by just 1โ2ยฐC above the summer maximum for several weeks, corals expel their zooxanthellae โ corals turn white (bleaching)
- Bleached corals are stressed but not dead โ if temperatures return to normal quickly, they can recover
- Prolonged bleaching โ coral death โ loss of entire reef ecosystem
- Great Barrier Reef (Australia) โ world’s largest coral reef; experienced mass bleaching in 1998, 2002, 2016, 2017, 2020, 2022 โ most severe bleaching on record in 2022
- India’s coral reefs: Lakshadweep Islands, Andaman & Nicobar Islands, Gulf of Mannar, Gulf of Kutch โ all experiencing bleaching events
- Lakshadweep experienced severe bleaching in 1998 and 2010; over 90% bleaching in some areas
๐ Ocean Warming + Acidification Double Threat: Corals face a double threat โ warming causes bleaching, while ocean acidification (see below) weakens their calcium carbonate skeletons. Together, these make coral survival increasingly difficult. Coral reefs support ~25% of all marine species despite covering less than 1% of the ocean floor.
๐งช Ocean Acidification
- Oceans absorb approximately 25โ30% of human COโ emissions each year
- COโ dissolves in seawater โ forms carbonic acid (HโCOโ) โ dissociates โ releases hydrogen ions โ pH drops
- Ocean pH has dropped from 8.2 (pre-industrial) to 8.1 (current) โ a 26% increase in acidity (pH is logarithmic)
- Projected to reach 7.95 by 2100 under high-emission scenarios
- Effects:
- Harms calcifying organisms โ corals, oysters, mussels, sea urchins, pteropods (sea butterflies) โ their shells dissolve in acidic water
- Disrupts fish behaviour and sensory systems
- Reduces ocean’s ability to absorb more COโ (positive feedback)
- Threatens the entire marine food web
โญ Exam Fact: Ocean acidification is sometimes called the “other COโ problem” or “evil twin of climate change.” The current rate of ocean acidification is the fastest in at least 300 million years. Pteropods (tiny sea snails) are called the “canary in the coal mine” for ocean acidification โ their shells are already dissolving in parts of the Southern Ocean.
๐ฆ Species Extinction & Biodiversity Loss
- Habitat loss โ rising temperatures make habitats unsuitable; species must migrate or face extinction
- Range shifts โ species moving poleward or to higher altitudes; some have nowhere to go (mountain-top species)
- Phenological mismatch โ timing of biological events (flowering, migration, breeding) shifts; predator-prey and pollinator-plant relationships disrupted
- Coral reef loss โ 25% of marine species depend on reefs; reef loss = mass marine extinction
- Polar species โ polar bears, Arctic foxes, penguins threatened by sea ice loss
- IPCC AR6: climate change is a major driver of biodiversity loss; at 1.5ยฐC, 4โ8% of species face high extinction risk; at 3ยฐC, 29% of species at risk
- India: Snow leopard, Himalayan brown bear, one-horned rhinoceros (flooding), Irrawaddy dolphin, Olive Ridley turtles (nesting beach loss) all threatened
๐พ Food Security
- Climate change threatens food production through multiple pathways
- Crop yield changes: wheat and maize yields declining in many regions; rice yields affected by heat stress during flowering
- Shifting agricultural zones: some regions become unsuitable; new areas may open up (e.g., higher latitudes)
- Water stress: changing rainfall patterns and glacier retreat reduce irrigation water availability
- Extreme events: floods, droughts, and heatwaves destroy crops
- COโ fertilisation effect: higher COโ can boost some crop yields (wheat, rice) but reduces nutritional quality (lower protein, zinc, iron)
- IPCC: global crop yields could decline by 2โ6% per decade while food demand increases by 50% by 2050
๐ India & Food Security: India is highly vulnerable โ agriculture employs ~45% of the workforce and contributes ~17% of GDP. Studies project wheat yields in India could fall by 6โ25% by 2100. Rice yields in eastern India could decline. The Indo-Gangetic Plain โ India’s breadbasket โ faces increasing heat stress and water scarcity.
๐ฎ๐ณ India-Specific Impacts of Climate Change
| Impact Area | Details |
|---|---|
| Monsoon Variability | Indian monsoon becoming more erratic โ longer dry spells interspersed with intense rainfall events; overall monsoon rainfall may increase but become more unpredictable; El Niรฑo years bring drought |
| Himalayan Glacier Retreat | Threatens long-term water security for 500+ million people dependent on Himalayan rivers; increased GLOF risk; Gangotri retreating ~22 m/year |
| Coastal Flooding | Mumbai, Chennai, Kolkata, Kochi at risk; Sundarbans islands submerging; 170 million coastal residents vulnerable |
| Heat Stress | India among most heat-stressed countries; 2022 heatwave caused crop failures and health emergencies; wet-bulb temperature approaching human survivability limits in some areas |
| Agricultural Disruption | Wheat and rice yields declining; shifting crop zones; water stress in Punjab and Haryana (groundwater depletion + reduced glacier melt) |
| Coral Reef Damage | Lakshadweep and Andaman reefs bleaching; threat to fisheries and tourism |
| Cyclone Intensification | Bay of Bengal cyclones intensifying rapidly; Arabian Sea cyclone frequency increasing (unusual) |
| Biodiversity Loss | Western Ghats, Eastern Himalayas (biodiversity hotspots) under threat; snow leopard, one-horned rhino, Olive Ridley turtles at risk |
โญ Wet-Bulb Temperature: A measure combining heat and humidity. At a wet-bulb temperature of 35ยฐC, the human body cannot cool itself through sweating โ survival is impossible beyond 6 hours even for healthy adults in shade. Parts of India, Pakistan, and the Persian Gulf are already approaching this threshold during extreme heat events.
โ Revision Checklist โ Effects of Climate Change
โ
Sea level rise = thermal expansion (~50%) + glacial/ice sheet melt
โ Current sea level rise rate = ~3.3โ3.7 mm/year (accelerating)
โ Most at risk: Maldives (avg 1.5 m elevation), Tuvalu, Bangladesh, Kiribati
โ Lohachara Island (Sundarbans) = first inhabited island submerged (2006)
โ Himalayan glaciers = “Third Pole” = 9,000+ glaciers = feed Ganga, Indus, Brahmaputra
โ Gangotri Glacier = source of Ganga = retreating ~22 m/year
โ GLOF = Glacial Lake Outburst Flood = increasing with climate change
โ Warmer atmosphere holds 7% more moisture per 1ยฐC โ heavier rainfall
โ Coral bleaching = water temp rises 1โ2ยฐC โ corals expel zooxanthellae โ turn white
โ India’s coral reefs = Lakshadweep, Andaman & Nicobar, Gulf of Mannar, Gulf of Kutch
โ Ocean acidification = COโ + seawater โ carbonic acid โ pH drops
โ Ocean pH = 8.2 (pre-industrial) โ 8.1 (current) = 26% more acidic
โ Harms calcifying organisms = corals, oysters, pteropods
โ Phenological mismatch = timing of biological events disrupted
โ COโ fertilisation = boosts some yields but reduces nutritional quality
โ India: monsoon variability + glacier retreat + coastal flooding + heat stress
โ Wet-bulb 35ยฐC = human survival limit = parts of India approaching this
โ India’s coastal population = 170 million people at risk
โ Current sea level rise rate = ~3.3โ3.7 mm/year (accelerating)
โ Most at risk: Maldives (avg 1.5 m elevation), Tuvalu, Bangladesh, Kiribati
โ Lohachara Island (Sundarbans) = first inhabited island submerged (2006)
โ Himalayan glaciers = “Third Pole” = 9,000+ glaciers = feed Ganga, Indus, Brahmaputra
โ Gangotri Glacier = source of Ganga = retreating ~22 m/year
โ GLOF = Glacial Lake Outburst Flood = increasing with climate change
โ Warmer atmosphere holds 7% more moisture per 1ยฐC โ heavier rainfall
โ Coral bleaching = water temp rises 1โ2ยฐC โ corals expel zooxanthellae โ turn white
โ India’s coral reefs = Lakshadweep, Andaman & Nicobar, Gulf of Mannar, Gulf of Kutch
โ Ocean acidification = COโ + seawater โ carbonic acid โ pH drops
โ Ocean pH = 8.2 (pre-industrial) โ 8.1 (current) = 26% more acidic
โ Harms calcifying organisms = corals, oysters, pteropods
โ Phenological mismatch = timing of biological events disrupted
โ COโ fertilisation = boosts some yields but reduces nutritional quality
โ India: monsoon variability + glacier retreat + coastal flooding + heat stress
โ Wet-bulb 35ยฐC = human survival limit = parts of India approaching this
โ India’s coastal population = 170 million people at risk