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Rising Seas and the Future of Coastal India

Takshasheela School of Civil Services
10 min read


Sea level rise, sinking land and shrinking shorelines are converging on India's coast, and the policy response is still catching up

India has a long, densely populated and economically vital coastline. Ports, fisheries, delta agriculture, mangroves, megacities and millions of livelihoods all sit within a few kilometres of the sea. For decades, coastal risk was discussed mainly through cyclones and floods. Increasingly, the more gradual threats matter just as much: seas that are rising faster, land that is sinking in some places, and shorelines that are being eaten away in others. For UPSC and APSC aspirants, this is a high-value topic that connects Geography, Environment, Disaster Management, Governance and International Relations. This article explains what is happening, what the evidence says, how India's rules respond, and where the gaps are.

1. Why Coastal India Is So Exposed

More than 200 million people in India live within 100 km of the coast, according to a 2026 study from the University of Rhode Island's Graduate School of Oceanography. That concentration of people, farmland, infrastructure and industry means that even modest changes in sea level, storm surge or shoreline position can have large consequences. Coastal states also host major deltas, estuaries, lagoons and mangrove systems, which protect the coast naturally but are themselves sensitive to rising water and reduced sediment supply.

Exposure is not limited to the big port cities. Mid-sized towns, fishing villages, island communities and agricultural deltas face risks of their own, often with weaker planning capacity and fewer resources to adapt.

2. What Is Rising: The Sea Level Evidence

Sea level rise has two parts. Global mean sea level rises because ocean water expands as it warms and because ice sheets and glaciers melt. Relative sea level, which is what coastal communities actually experience, also depends on whether the local land is rising, stable or sinking. The distinction matters greatly for India, as the next section shows.

Indicator What the data says
Global rate of rise Reported to have accelerated from about 2.1 mm a year (1993 to 2002) to about 4.7 mm a year (2015 to 2024), with a record rise of about 6 mm in 2024
Rise along the Indian coast About 1.70 mm a year, or roughly 8.5 cm over 50 years, as stated by the Environment Ministry in Parliament
North Indian Ocean, 2003 to 2013 About 6.1 mm a year, according to the same ministry reply, reflecting faster recent rise
People at risk Projections cited in recent reporting suggest about 45 million Indians could be at risk from sea level rise by 2050

The gap between the long-term Indian average of 1.7 mm a year and the much higher recent regional rate shows why long averages can understate the present trend. Projections for the end of the century depend heavily on future emissions. The IPCC's Sixth Assessment Report gives a likely global range of roughly 0.3 to 1 metre by 2100, with the lower end under strong emission cuts and the upper end under very high emissions, and it does not rule out higher outcomes if ice sheets destabilise.

3. The Hidden Multiplier: Sinking Land

A study led by the University of Rhode Island, published in Geophysical Research Letters and reported in March 2026, analysed eight years (2016 to 2024) of Sentinel-1 satellite radar data for areas within 100 km of India's coastline. Its main findings were:

  • About 8.5 million residents live in coastal areas that are sinking faster than 5 mm a year.
  • In five major east coast deltas, subsidence reaches up to 20 mm a year.
  • Hotspots include Ahmedabad, Chennai, Amaravati, Kochi, Kakinada and Kolkata, and the researchers stress that many mid-sized cities are affected, not only megacities.
  • The main driver is believed to be groundwater extraction, which compacts fine-grained sediments and lowers the land surface.

The implication is important. Where land sinks at 5 to 20 mm a year, relative sea level rises far faster than the 1.7 mm a year regional average, and flood risk grows accordingly. This also means part of the problem is in local hands: managing groundwater withdrawal is a coastal adaptation measure, not only a water policy.

4. Eroding Shores

The National Centre for Coastal Research (NCCR) assessed India's mainland shoreline from 1990 to 2018 using satellite imagery and field surveys. As told to Parliament by the Environment Ministry:

  • About 33.6 percent of the coastline was eroding.
  • About 26.9 percent was accreting, meaning it was gaining land.
  • About 39.6 percent was stable.

Erosion is highly uneven. In Karnataka, for example, reported figures show 48.4 percent of the Dakshina Kannada coast and 34.7 percent of the Udupi coast eroding, against 12.3 percent in Uttara Kannada. Reporting based on NCCR work also cites about 234 square kilometres of land lost to erosion between 1990 and 2016, with a similar area gained elsewhere.

The Sundarbans and Ghoramara: A Warning

Ghoramara Island in the Sundarbans shows what chronic erosion looks like. Studies cited by India Water Portal report that the island shrank from about 7.2 square kilometres in 1972 to about 3.6 square kilometres in 2022, roughly half in 50 years, and could fall to about 2.6 square kilometres by 2032. Around 3,000 people were displaced in 2016. Some families who earlier moved from the vanished Lohachara Island were displaced a second time. The causes include rising relative sea level and sediment starvation linked to upstream engineering in the Hooghly estuary, and embankments have often failed or worsened scouring.

5. Cities and Ecosystems at Risk

A 2024 report from the Centre for Study of Science, Technology and Policy (CSTEP) mapped sea level rise scenarios and inundation for 15 Indian coastal cities and towns. Its press release highlights Haldia, Udupi, Panaji and Yanam as places that would face inundation, and points to impacts on water, agriculture, forests and biodiversity, and health. Beaches, backwaters and mangroves are especially vulnerable, with consequences for tourism and for the natural protection these systems provide.

Combine this with the subsidence hotspots and a pattern emerges: Kolkata, Chennai, Kochi and several smaller east coast cities face compound risk from sea level rise, sinking ground, storm surge and, in some cases, river flooding at the same time.

6. India's Policy Framework and Its Gaps

The Coastal Regulation Zone Notification, 2019

The CRZ Notification 2019, issued under the Environment (Protection) Act, regulates activity along the coast. Its main features include:

  • CRZ-I covers ecologically sensitive areas. It is split into CRZ-IA (mangroves, coral reefs, sand dunes, turtle nesting grounds and similar features) and CRZ-IB (the intertidal zone between low and high tide lines).
  • CRZ-IV covers the Andaman and Nicobar Islands, Lakshadweep and small islands not placed in other categories.
  • No-development buffers are measured from the high tide line, reported as 50 metres in densely populated rural areas and 200 metres elsewhere in the relevant category.
  • Regulated projects generally need CRZ clearance before they begin.

Critics argue that successive amendments have weakened protection in favour of commercial interests. Draft amendments notified on 1 November 2021, for example, proposed delegating clearance for small projects to state authorities and exempting exploratory oil and gas drilling outside CRZ-IA from clearance. Reporting on earlier consultations also alleged that most objections raised by fishing communities and environmental groups were disregarded.

Hazard Line and Integrated Coastal Zone Management

The Survey of India has mapped a hazard line that accounts for sea level rise and shoreline change, intended for disaster management and land-use planning. It is not yet used to define no-build zones. India also uses Integrated Coastal Zone Management (ICZM) as a core approach, combining coastal law, hard engineering such as seawalls, soft engineering such as beach nourishment, and nature-based solutions such as mangrove restoration.

Where the Gaps Are

  • Fragmentation: A review in Frontiers in Marine Science argues that India lacks a unified framework that brings its coastal adaptation actions together, leading to inefficient spending and risk of maladaptation.
  • Displacement: India has no comprehensive law or policy category for people displaced gradually by erosion or rising water. They are neither classic disaster victims nor project-affected persons. Fiji, by contrast, wrote planned relocation into its Climate Change Act (2021) and created a relocation trust fund.
  • Hard engineering: Embankments and seawalls can protect one stretch while accelerating erosion elsewhere.
  • Planning: Shoreline change and subsidence projections are not consistently built into district and state development plans.

7. The Global Dimension

According to reporting based on the Indian Express, the UN General Assembly adopted its first declaration on rising sea levels on 24 September 2026. It affirms that states losing territory to sea level rise keep their statehood, sovereignty and stable maritime zones, an issue that matters most for low-lying island nations. For India, the larger concern is adaptation finance. Developing countries are reported to need over 310 billion US dollars a year by 2035 for adaptation, against about 26 billion dollars provided in 2023, and India called the 300 billion dollar goal agreed at COP29 too little and too distant. India continues to anchor its position in the principle of common but differentiated responsibilities and respective capabilities. The next high-level discussion is expected at COP31 in Antalya, Turkiye, from 9 to 20 November 2026.

8. The Way Forward

  • Treat subsidence as a coastal risk: Regulate groundwater extraction in coastal cities and deltas, and include subsidence data in flood and land-use planning.
  • Use the hazard line in planning: Integrate it into zoning and no-build decisions rather than leaving it advisory.
  • Prefer nature-based protection: Restore mangroves, wetlands and dunes, and manage sediment at river-basin level, since coast and catchment are linked.
  • Plan retreat where needed: Create a legal and financial framework for planned relocation with housing, livelihoods and secure tenure.
  • Unify the framework: Bring CRZ, ICZM, disaster management and urban planning into one coherent adaptation strategy with clear institutional responsibility.
  • Protect livelihoods: Involve fishing and coastal communities in decisions, since their consent and knowledge determine whether measures work.
  • Press for finance and technology: Pursue predictable adaptation finance in international negotiations.

9. Quick Revision for Exams

Topic Points to remember
Relative sea level rise Combines global rise with local land movement such as subsidence
NCCR shoreline assessment (1990 to 2018) 33.6 percent eroding, 26.9 percent accreting, 39.6 percent stable
Subsidence study (2026) Up to 20 mm a year in east coast deltas; groundwater extraction is the main driver
CRZ Notification 2019 Categories CRZ-I (IA, IB), II, III, IV; buffers measured from the high tide line
Hazard line Survey of India mapping that accounts for sea level rise; not yet used for no-build zones
Ghoramara Island Sundarbans island that has lost roughly half its area in 50 years
Policy gap No law for people displaced gradually by erosion; fragmented adaptation framework
International UNGA declaration on sea level rise (September 2026); COP31 in Antalya, November 2026; CBDR-RC

Possible mains questions:

  • Discuss how land subsidence and sea level rise together increase coastal risk in India, and suggest measures.
  • Critically examine whether the CRZ Notification 2019 adequately protects India's coast against climate risks.
  • Why is planned relocation a governance challenge for climate-displaced coastal communities in India?
  • Evaluate the case for nature-based solutions over hard engineering along India's coastline.

10. Final Thoughts

The story of Coastal India is not a single rising line on a graph. It is rising water, sinking ground, shifting sediment and thin planning capacity acting together, with the heaviest burden falling on fishing communities, delta farmers and island residents. The good news is that many drivers are within reach of policy: groundwater, mangroves, zoning, relocation and finance. For aspirants, the strongest answers will connect the science to governance, using specific data points, naming the institutions involved, and proposing balanced, implementable solutions.

Sources

Information as of 22 October 2026, compiled from the sources listed above. Figures, court and policy positions, and international negotiations may change, so verify the latest details from official sources before using them in an examination answer.

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