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Subject: Geography

  • The groundwater potential of the gangetic valley is on a serious decline. How may it affect the food security of India?

    The Indo-Gangetic Valley is home to one of the world’s most prolific alluvial aquifer systems. Yet, according to the United Nations (2025-26) reports, several regions in this basin have crossed the “groundwater depletion tipping point.”

    Declining groundwater potential

    Nationwide, India extracts approximately 247 BCM of groundwater annually, more than China and the US combined.

    Groundwater storage in the Ganga basin is declining at an average rate of 2.6 cm per year. (CGWB)

    In Punjab and Haryana, nearly 78% of assessment units are categorized as “over-exploited.”

    Reasons Behind the Decline

    Green Revolution Legacy-The shift to High-Yielding Varieties (HYV) required 3-4 times more water than traditional seeds.

    Faulty Cropping Patterns-Cultivation of water-guzzling crops like Paddy in semi-arid regions (Punjab/Haryana) where they are not ecologically suited.

    Energy Subsidies-Free or heavily subsidized electricity leads to “blind pumping” in states like Punjab and Haryana.

    Inadequate Regulation-Under the Indian Easements Act 1882, groundwater is tied to land ownership, allowing landowners to extract unlimited water without legal penalty.

    Rapid urban expansion in cities like Delhi, Kanpur, and Patna has reduced the “pervious” area available for natural recharge.

    Climate Change & Monsoonal Shifts-Erratic rainfall patterns mean shorter, more intense bursts of rain that run off rather than seeping into the ground.

    Inefficient Irrigation-Traditional Flood Irrigation methods result in nearly 40% water wastage through evaporation and runoff.

    Deforestation in Catchment Areas-Loss of forest cover in the Himalayan foothills (Shivaliks) has disrupted the natural hydrological cycle that feeds the Gangetic aquifers.

    Industrial Contamination-Discharge of untreated effluents reduces the “potable” potential of the remaining groundwater.

    Population Pressure-With the IGP being one of the most densely populated regions globally, domestic demand has surged, competing directly with agriculture.

    Impact on Food Security

    Yield Reductions-Studies show a 1-meter decline in the water table can lead to an 8% reduction in food grain production.

    Threat to Staples-Punjab and Haryana provide 50% of India’s rice and 85% of its wheat, depletion here directly threatens the National Buffer Stock.

    Increased Cost of Cultivation-Farmers must drill deeper (up to 300-500 ft) and install expensive submersible pumps, leading to rural indebtedness.

    Punjab and Haryana supply a major portion of wheat and rice for the PDS. Reduced grain output affects government stocks.

    Food Inflation-Reduced supply and higher production costs lead to a spike in market prices, making food unaffordable for the poor.

    Quality Degradation (Nutritional Security)-As water levels drop, concentrations of Arsenic and Uranium increase. These enter the food chain, compromising food safety.

    Land Degradation-Excessive groundwater use leads to soil salinization, turning once-fertile alluvial tracts into barren “Usar” land.

    Reduced Cropping Intensity-Farmers who previously grew three crops a year (Zaid, Kharif, Rabi) are being forced to skip seasons due to dry wells.

    Vulnerability of Small Farmers-While wealthy farmers can afford deeper wells, marginal farmers lose access entirely, leading to “de-peasantization” and migration.

    Climate Instability-Without groundwater, Indian agriculture becomes more dependent on the vagaries of the monsoon.

    Way Forward

    Crop Diversification-Aggressively shifting from Paddy to Millets (Shree Anna), pulses, and oilseeds in over-exploited blocks.

    Micro-Irrigation-Scaling up the “Per Drop More Crop” initiative to make drip and sprinkler irrigation mandatory for water-intensive crops.

    Managed Aquifer Recharge (MAR)-Utilizing the Mission Amrit Sarovar to rejuvenate 75,000+ local ponds to act as recharge pits.

    Power Reforms-Transitioning from free electricity to Direct Benefit Transfer (DBT) for electricity.

    Unified Water Governance-Implementing the Mihir Shah Committee recommendations to merge the CGWB and CWC into a single National Water Commission.

    Community-Led Management-Scaling the Atal Bhujal Yojana model where villagers prepare “Water Security Plans” based on their local water budget.

    Legal Reform-Updating the 19th-century Easement Act to treat groundwater as a “Common Pool Resource” rather than private property.

    Aligning agricultural policies with ecological limits and climate resilience can ensure long term food security.

    Indian Geography

  • What is a twister? Why are the majority of twisters observed in areas around the Gulf of Mexico?

    Key Features of a Twister

    Funnel-shaped cloud – Visible condensation funnel extending downward.

    Very high wind speeds – Can exceed 300 km/h (EF5 category).

    Short duration – Typically lasts minutes but causes intense damage.

    Narrow path of destruction – Damage track often a few hundred meters wide.

    Associated with supercell thunderstorms

    Low pressure core – Central pressure drop causes debris uplift.

    Occurs mostly in mid-latitudes – Especially continental interiors.

    Formation Process of a Twister

    Warm, moist air near the surface rises rapidly.

    Cold, dry air above descends below.

    Wind shear develops – Change in wind speed and direction with height.

    Horizontal rotation forms in the lower atmosphere.

    Updraft tilts rotation vertically, forming a mesocyclone.

    Supercell thunderstorm develops.

    A funnel cloud forms and extends to ground, becoming a tornado.

    Reasons for Majority of Twisters Around the Gulf of Mexico

    Continuous supply of warm, moist air – Gulf waters average 25-30°C.

    Collision of contrasting air masses – Warm Gulf air meets cold Canadian air over central U.S.

    No Latitudinal Barriers- Unlike Europe’s Alps, North America has no east-west mountain ranges to block the collision of these contrasting air masses.

    Low-Level Jet Streams from the Gulf provide the necessary wind shear to initiate rotation near the ground.

    Dryline effect – Dry air from Rockies creates a sharp moisture gradient leading to storm development.

    The Great Plains and Mississippi Valley offer a smooth “runway” that prevents the disruption of rotating storm structures.

    Proximity to Tornado Alley – Central U.S. records ~75% of world’s tornadoes.

    The high frequency of thunderstorms in the gulf region creates tornados. 83% of Gulf hurricanes since 1950 have produced at least one tornado.

    As climate variability enhances the frequency and intensity of tornados, advanced radar detection and robust disaster preparedness is needed for disaster risk reduction.

  • What is sea surface temperature rise? How does it affect the formation of tropical cyclones?

    Sea Surface Temperature (SST) rise refers to the increase in temperature of the upper layer of ocean water. It is a critical indicator of the Earth’s climate health

    Causes of sea surface temperature rise

    Greenhouse gas emissions – Eg- Atmospheric CO₂ crossed 425 ppm.

    Global warming trend – Eg- Earth warmed ~1.44°C since pre-industrial levels. (IPCC)

    Marine heatwaves – Persistent abnormal warming events.

    Weakening ocean circulation reduces heat redistribution. Eg- Slowing Atlantic Meridional Overturning Circulation (AMOC).

    El Niño events – Periodic warming of Pacific surface waters.

    Declining polar ice cover – Reduced albedo effect increases absorption.

    Ocean Stratification- As surface water warms, it becomes lighter and fails to mix with deeper, cooler water

    Impact of SST rise on formation of tropical cyclones

    Minimum SST of 26.5°C was required for a cyclone to form. Rising sea temperature has led to

    Cyclones in South Atlantic and higher latitudes of the Pacific

    Arabian Sea witnessing more intense storms. Eg- Cyclone Nisarga (2020) near Maharashtra coast.

    Enhanced evaporation – Warmer oceans increase moisture supply. Eg- Rapid moisture buildup before Cyclone Amphan (2020).

    Rapid Intensification (RI)- High SSTs provide an explosive amount of latent heat. Eg- Hurricane Milton (2024) jumped from Category 1 to Category 5 in under 24 hours.

    Greater Storm Size- Eg- Super Cyclone Amphan (2020) covered almost the entire Bay of Bengal during its peak.

    For every 1°C of SST rise, the air holds 7% more water vapor. This leads to greater rainfall during cyclonic activity.

    High SSTs allow storms to carry their moisture further inland before dissipating. Eg- Hurricane Harvey in Texas

    Higher storm surge risk – Combined SST rise and sea-level rise amplify flooding. Eg- Cyclone Idai (2019) caused severe coastal inundation.

    Shift in cyclone tracks and behavior due to altered SST gradients. Eg- Increasing westward shift of North Indian Ocean cyclones.

    Addressing this challenge requires a multi-layered climate and disaster strategy

    Mitigate greenhouse gas emissions

    Strengthen ocean monitoring systems

    Improve cyclone early warning systems

    Protect natural buffers. Eg- mangroves

  • What is the phenomenon of ‘cloudbursts’? Explain.

    IMD defines cloudburst as an extreme weather event involving very high-intensity rainfall (often >100 mm/hour) over a small geographical area (20-30 sq. km.) within a short duration.

    Orographic Uplift

    Moist air masses are forced to rise abruptly when they encounter steep mountain slopes.

    Rapid ascent causes condensation and release of latent heat, intensifying convection.

    Strong Convective Clouds (Cumulonimbus) up to 12-15 km.

    Moisture Supply from Monsoon Systems enhances instability.

    When updrafts weaken, large volumes of accumulated rainwater are released at once, causing cloudburst-like rainfall.

    Occurrence of cloudburst in the Indian Subcontinent

    Himalayan and Western Ghat Topography – Steep slopes promote rapid vertical uplift.

    Monsoon Dynamics – High atmospheric moisture during June-September.

    Climate Change – Rising temperatures increase atmospheric moisture-holding capacity. Eg- every 1°C rise lets air hold ~7% more moisture.

    Land-Use Changes – Deforestation, slope cutting, and urbanisation increase runoff and disaster impact.

    Mitigation measures

    Structural

    Engineering solutions – Retaining walls, slope drainage, rock bolting, geo-textiles,

    Nature based solutions – Afforestation in himalaya

    Non-Structural

    Expansion of multi-hazard insurance

    Disaster resilient urban planning (Mishra committee on Joshimath crisis)

    The Sendai Framework’s proactive approach is essential for making Bharat a ‘weather-ready and climate-smart’ nation.

    Geomorphology

  • What are aurora australis and aurora borealis? How are these triggered?

    An aurora is a natural luminous phenomenon seen in high-latitude skies, caused by the interaction between charged particles from the Sun and Earth’s upper atmosphere, producing dynamic light displays in various colors.

    Aurora Australis (Southern Lights)

    Occurs in the Southern Hemisphere – Visible near the Antarctic Circle.

    Observed in countries likeAntarctica, Tasmania (Australia), New Zealand, and the southern tip of Argentina.

    Forms luminous arcs and curtains – Green, red, purple colors dominate.

    Best viewed during the Southern Hemisphere’s winter (May to September) due to the long hours of darkness.

    Aurora Borealis (Northern Lights)

    Occurs in the Northern Hemisphere – Visible near the Arctic Circle.

    Observed in countries like – Norway, Sweden, Finland, Canada, Alaska.

    Displays dynamic wave-like patterns – Curtains, spirals, and arcs.

    March and September equinoxes are peak viewing times due to the Russell-McPherron effect, which allows solar energy to enter the atmosphere more easily.

    Triggers of Auroras

    Solar Activity

    The Sun’s corona constantly releases a stream of protons and electrons at speeds up to 900 km/s.

    These particles hit the Magnetosphere (Earth’s magnetic shield), which deflects most of them.

    Magnetic lines guide particles poleward as Earth’s magnetic field lines are weakest and more vertical at the North and South Poles.

    Acceleration (Birkeland Currents)- Particles gain speed as they spiral down the field lines toward the Ionosphere.

    Atmospheric Collision- Charged particles collide with gas atoms (Oxygen and Nitrogen) in the Thermosphere (approx. 100km-400km up).

    The collision transfers energy to the gas atoms, moving their electrons to a higher-energy state.

    These atoms release that energy as a photon (a packet of light).

    Color Differentiation- Oxygen produces green and red, Nitrogen produces blue or purple light.

    They illustrate the protective role of the magnetosphere while producing one of the most visually stunning atmospheric phenomena.

  • Give a geographical explanation of the distribution of off-shore oil reserves of the world. How are they different from the on-shore occurrences of oil reserves?

    Petroleum reserves are found in sedimentary basins, where organic matter is trapped under pressure. Offshore reserves account for ~30% of global crude oil production. Their distribution is linked to continental shelf geology, passive margins, and deep-water basins.

    Geographical distribution

    The Persian Gulf (Middle East)- result of the collision between the Arabian and Eurasian plates, which created perfect “anticline” traps for oil. Eg- Safaniya field (Saudi Arabia), largest offshore oil field in the world.

    The Gulf of Mexico (North America)- It is characterized by salt domes that trap oil in the surrounding porous rock.

    The North Sea (Europe)- Situated between the UK, Norway, and Denmark. This region is a rift basin, with deep depressions where organic matter could settle.

    The South Atlantic Margins (Brazil & West Africa)- formed when South America and Africa drifted apart.

    Southeast Asia & India- in the South China Sea and India’s Mumbai High and Krishna-Godavari (KG) Basin

    Difference between off-shore and on-shore oil reserves

    Implications of uneven distribution of mineral oils in the world

    Energy security challenges – Oil-deficient countries face high import bills and current account deficits. Eg- India imports ~85% of its crude oil requirement.

    Resource Curse in Oil-rich Nations (Paradox of Plenty) – Overdependence on oil leads to limited economic diversification. Eg- Venezuela’s economic crisis.

    Energy trade is one of the key drivers of global geopolitics. Eg- US sanctions on Russian and Iran oil trade

    Competition for oil resources leads to wars and regional instability. Eg- Gulf Wars, Saudi-Iran rivalry.

    Oil-rich regions face oil spills, land degradation, and marine pollution. Eg- Niger Delta pollution.

    Global Carbon Emissions – oil and gas industry is responsible for over 5 billion tonnes of CO2 equivalent in direct emissions annually (15% of total energy-related emissions)

    In the long run, reducing oil dependence through clean energy, strategic reserves, and diversified supply chains is essential for ensuring equitable and sustainable global development.

  • How can Artificial Intelligence (AI) and drones be effectively used along with GIS and RS techniques in locational and areal planning?

    Locational and aerial planning involves selecting optimal sites for infrastructure and managing land use through spatial analysis. The integration of AI, drones, GIS, and Remote Sensing makes planning more efficient, accurate, and sustainable.

    Technological Synergy

    Drones & RS- Satellites provide the macro-view (regional scale), while Drones provide the micro-view (site scale) with high-resolution imagery and LiDAR.

    GIS acts as the central “brain” where all spatial data is layered, stored, and visualized.

    AI processes the massive data from drones/RS to automatically detect patterns, classify land, and predict future trends.

    Role of AI with GIS and RS in Planning

    Automated Land Use Classification- Eg- ISRO’s Bhuvan portal uses AI to automate the Land Use Land Cover (LULC) mapping across India.

    Infrastructure Corridor Optimization- Eg- The PM Gati Shakti platform integrates 200+ GIS layers to plan multi-modal connectivity projects across India.

    Predictive Urban Growth- AI analyzes historical RS data to predict future urban sprawl, helping in proactive zoning.

    Optimal Site Selection for Renewables- AI evaluates GIS layers like slope, solar radiation, and grid proximity to identify high-yield locations.

    Traffic and Mobility Planning- AI analyzes real-time GIS traffic data to optimize the location of new flyovers or metro stations.

    Environmental Risk Assessment- AI simulates flood or landslide scenarios based on RS topographical data to designate “no-build” zones.

    Precision Agriculture Planning- AI analyzes multispectral RS data to determine the best locations for warehouses based on crop yield forecasts. Eg- FASAL project uses AI to forecast district-level yields.

    Illegal Construction Detection- AI compares time-series satellite images to automatically flag unauthorized changes in land use.

    Retail and Logistics Locational Planning- Eg- Amazon and Flipkart use spatial AI to decide the location of “Dark Stores” for 10-minute deliveries.

    Role of Drones with GIS and RS in Planning

    High-Resolution Cadastral Mapping- Drones create centimeter-level accurate maps for property titling.

    3D Digital Twins of Cities- Drones use LiDAR to create 3D replicas of urban areas for detailed architectural planning.

    Real-Time Construction Monitoring- Eg- NHAI has mandated drone surveys for all highway projects to monitor progress.

    Disaster Damage Assessment- In areas inaccessible to RS due to cloud cover, drones provide immediate imagery for relief planning.

    Mining Area Surveillance- Wg- using drones to prevent illegal iron ore mining.

    Coastal Zone Management- Drones map shoreline erosion and mangrove health with high precision for environmental planning.

    Transmission Line Planning- Eg- PowerGrid Corporation of India uses drones for the inspection and locational planning of pylons in hilly terrains.

    Hydrological Planning- Eg- Under the Jal Shakti Abhiyan, drones map micro-watersheds for water conservation planning.

    Challenges

    High initial cost of technology and data processing infrastructure

    Shortage of skilled geospatial and AI professionals

    Data integration issues between multiple agencies due to different formats and standards delay implementation.

    Regulatory restrictions on drone operations

    Data privacy – High-resolution mapping of urban areas raises privacy issues.

    Inadequate real-time data sharing due to low inter-agency coordination

    Lack of decentralised planning capacity at local level – ULBs and PRIs lack funds and functionaries.

    Way Forward

    Implement National Geospatial Policy 2022 for open access and standardised datasets

    Capacity building at state and local levels – Establish district-level geospatial planning units

    Promote public-private partnerships for geospatial infrastructure

    Integrate Bhuvan, Digital India Land Records, and urban GIS databases

    Simplify drone regulations under Drone Rules 2021 for planning use


    These measures can improve evidence-based spatial planning and resource optimisation in India.

    Environmental Geography

  • Discuss the distribution and density of population in the Ganga River Basin with special reference to land, soil and water resources.

    The Ganga River Basin houses around 43% of India’s population (600 million) in about 26% of its geographical area. The average population density exceeds 520 persons/km².

    Distribution and Density of Population

    Upper Ganga Basin

    Characterized by low density (approx. 150-300 persons/km²).

    Rugged terrain and steep slopes restrict large-scale habitation to river valleys like Dehradun and Haridwar.

    Middle Ganga Plain – “demographic heartland” with very high density (800-1,100+ persons/km²).

    Lower Ganga Plain – extremely high density (exceeding 1,000-1,300 persons/km²), particularly in the deltaic regions and the Kolkata Metropolitan Area.

    Impact of Land on Distribution and Density of Population

    Extensive level plains support agriculture, transport, and urban expansion. Eg- eastern Uttar Pradesh and north Bihar.

    A high proportion of cultivable land supports intensive agricultural activity. Eg- Rice-wheat belt of the middle Ganga plain.

    Deltaic plains – Urban and industrial concentration. Eg- Kolkata-Howrah region in the lower Ganga plain.

    Piedmont and Tarai zone – Forests converted into agricultural land increased settlement. Eg- Tarai region of Uttarakhand and Uttar Pradesh.

    Himalayan Foothills-In the Upper Basin (Uttarakhand), rugged terrain restricts population to valley floors. Eg- Dehradun and Haridwar

    Ease of Habitation-The vast, flat alluvial plains allow for the construction of dense transport networks. Eg- National Highway 19 corridor connects mega-cities like Delhi, Kanpur, and Kolkata.

    Gentle Slope-A gradient of barely 20cm/km facilitates large-scale urban sprawl. Eg- The rapid expansion of cities like Noida and Ghaziabad

    Doab Regions-The fertile land between two rivers (Doabs) shows the highest density. Eg- The Ganga-Yamuna Doab

    Impact of soil on distribution and density of population

    Alluvial Dominance-Over 70% of the basin is covered by nutrient-rich alluvium, supporting 80% of its population.

    Soil suitable for diverse crops – Rice, wheat, sugarcane, pulses and jute support a dense population. Eg- Jute cultivation in West Bengal delta.

    Khadar (New Alluvium)-Annually replenished by floods, these soils support intensive agriculture. Eg- North Bihar plains sustain a density of over 1,100 persons/km² due to its high productivity.

    Bhangar (Old Alluvium)-Stable, older soils support the wheat-sugar cane belt and high rural density of Western Uttar Pradesh.

    Multi-cropping Potential-Eg- Farmers in the Lower Ganga Basin (West Bengal) grow three rice crops (Aman, Aus, Boro), sustaining very high rural populations.

    Deltaic Silt-The nutrient-dense silt in the Sunderbans and Bengal delta supports high-intensity fishing and farming. Eg- High densities in districts like South 24 Parganas despite the risk of cyclones.

    Impact of water on distribution and density of population

    Perennial river system – Reliable water for domestic and agricultural use supports dense settlements. Eg- Kanpur on Ganga bank.

    Extensive canal irrigation supports agricultural intensification and increases rural density. Eg- Upper Ganga Canal in western Uttar Pradesh.

    Groundwater Availability-Eg- The widespread use of tubewells in the Bihar plains allows for dense human clusters away from the main river.

    Inland water transport supports urban growth. Eg- Eg- National Waterway-1 along the Ganga.

    Major Challenges

    Very high population pressure on land – Average landholding size in Bihar and eastern UP is less than 1 hectare.

    Frequent floods – Displacement and loss of livelihood. Eg- Annual floods in north Bihar.

    Groundwater depletion – Over-extraction for irrigation in western and central UP.

    Water pollution – Eg- Industrial and domestic waste in Kanpur-Varanasi stretch.

    Declining soil fertility due to overuse of fertilisers. Eg- Green Revolution areas of western UP.

    Unplanned urbanisation – Pressure on land and water resources

    Climate variability – Irregular monsoon and heat stress impact agriculture productivity and public health.

    Efficient land use planning, flood management, groundwater regulation, and soil conservation are essential for maintaining the region’s demographic and ecological balance.

    Society

    Salient Features

  • Explain briefly the ecological and economic benefits of solar energy generation in India with suitable examples.

    India has emerged as a global leader in solar energy with over 140 GW of installed solar capacity (Nov 2025) and ranks 3rd in the world in solar capacity and generation.

    Ecological Benefits

    Carbon Sequestration

    By replacing coal-fired thermal power, which is the primary source of CO-2 emissions. Every 1 GW of solar power reduces CO2 emissions by approximately 1.5 million tonnes annually.

    Supports India’s NDC targets – 500 GW non-fossil capacity by 2030 and net-zero by 2070.

    Water Conservation – Use 95% less water than thermal power plants. Shifting to solar saves roughly 2.5 liters of water per kWh generated.

    Preservation of Fragile Ecosystems – Installing panels on reservoirs reduces water evaporation and algae growth. Eg- Omkareshwar Floating Solar Park (Madhya Pradesh).

    Agrivoltaic Biodiversity – “Solar farming” allows crops to grow beneath panels, creating a micro-climate that reduces soil moisture loss.

    Reduction Air Pollution – Unlike fossil fuels, solar generation releases zero SOx, NOx, or particulate matter (PM 2.5).

    Soil Reclamation – Solar parks built on saline or degraded “wastelands,” prevent further soil erosion. Eg- Khavda Hybrid Park in the Rann of Kutch

    Transition to Circular Economy – Eg- Draft Solar Waste Management Rules mandate recycling of end-of-life panels.

    Protection of Glacial Regions – Eg- Solar projects in Ladakh (13 GW planned) can reduce black carbon deposits on glaciers, which otherwise accelerate melting.

    Economic Benefits

    Cost Savings for Households – Solar tariffs are lower compared to coal based power.

    Reduction in Energy Import Bill – Solar energy helped India save roughly $4.2 billion in fuel costs in 2024-25, strengthening the Current Account Balance.

    Boost to Domestic Manufacturing (PLI Scheme) – Solar manufacturing capacity jumped from 38 GW to 74 GW in 2025, attracting ₹52,900 crore in fresh private investment.

    Agricultural Income Diversification- Under PM-KUSUM Component A, farmers can earn income by installing solar plants on unproductive land.

    Attraction of Global FDI – 100% FDI under the automatic route has made India a top destination for ESG-focused global funds.

    Rural Electrification – Solar micro-grids provide 24/7 power to remote villages where grid extension is expensive.

    Infrastructure Development – Mega solar parks bring roads, water, and connectivity to previously isolated regions.

    Export Potential– India exported $1.5 billion worth of solar equipment in 2025.

    Challenges in Solar Energy Generation

    Intermittency and Storage Gap- shortage of Battery Energy Storage Systems (BESS)

    Land Acquisition Hurdles for Mega-parks

    Lack of grid connectivity

    Import dependency- India still imports over 90% of its wafers and ingots from China.

    Limited recycling infrastructure creates a toxic waste risk (lead and cadmium).

    Poor Financial Health of DISCOMs- delayed payments to solar developers and deterring investment.

    Steps Taken by Governments

    PM-Surya Ghar- Muft Bijli Yojana to solarize 1 crore households by 2027

    Solar Park Scheme- A target of 40 GW across 50+ parks by March 2026.

    PM-KUSUM- Solarizing over 30 million irrigation pumps.

    PLI Scheme- to boost domestic manufacturing of high-efficiency solar modules

    A balanced strategy focusing on decentralised solar, grid expansion, storage systems, and region-specific planning is essential to achieve Panchamrit Targets.

  • How are climate change and the sea level rise affecting the very existence of many island nations? Discuss with examples.

    As per the IPCC, global mean sea level rose by 0.20 m between 1901 and 2018. It has projected a global mean SLR of 1.3 to 1.6 m by 2100 under the high-emission scenario.

    Permanent submergence of land – Eg- Kiribati has already seen two small uninhabited islets (Tebua Tarawa and Abanuea) disappear underwater.

    Coastal erosion – Wave action and storm surges remove shoreline. Eg- Shoreline retreat in the Maldives.

    Salinisation of freshwater lenses – Sea water enters groundwater and contaminates wells leading to drinking water shortage.

    Frequent flooding during high tides and storms can lead to large scale displacement. Eg- “King tide” flooding in Tuvalu.

    Damage to housing and public infrastructure – Eg- Majuro Airport in the Marshall Islands frequently faces flooding

    Loss of agriculture – Salinity affects soil fertility and traditional crops. Eg- Taro cultivation affected in Kiribati and Tuvalu.

    Coral reef degradation – Ocean warming and acidification damage reefs that act as wave barriers. Eg- Coral bleaching in Fiji and Maldives.

    Impact on fisheries – Changes in ocean temperature and reef systems reduce fish catch, impacting livelihood

    Climate-induced migration – Eg- Kiribati purchased land in Fiji for future resettlement.

    Way Forward

    Hard Engineering Measures

    Seawalls to block wave attack.

    Groynes – Trap sand and widen beaches. Eg- Puducherry groyne field.

    Breakwaters – Offshore barriers that reduce wave energy. Eg- Chennai port.

    Revetments – Sloped rock armour to absorb wave impact.

    Soft Engineering Measures

    Mangrove Restoration – Eg- MISHTI-based efforts in Sundarbans.

    Coral and Seagrass Restoration – Eg- Andaman reef rehabilitation.

    Integrated Coastal Zone Management (ICZM)

    Ecosystem-Based Coastal Planning – Combines geomorphology, ecology and socio-economic factors.

    Regulatory Tools (CRZ Norms) – no-development zones and hazard mapping reduce vulnerability.

    Early Warning SystemsINCOIS alerts for timely action.

    Strengthening coastal resilience and climate mitigation is essential to safeguard communities and advance SDG 13 (Climate Action) and SDG 14 (Life Below Water).

    Water