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1st September 2025 (15 Topics)

Rising Seas and Coral Reefs

Context:

A recent study using coral microatolls in the Maldives has reconstructed sea-level history over 90 years, showing that sea-level rise in the Indian Ocean began as early as the late 1950s, much earlier than previously believed.

Key Dimensions of the Issue

Sea-Level Rise in the Indian Ocean

  • Indian Ocean average rise: ~3.3 mm/year, higher than the global average.
  • Total increase over the last half-century: 30–40 cm.
  • Acceleration observed:
    • 1930–1959: 1–1.84 mm/year.
    • 1960–1992: 2.76–4.12 mm/year.
    • 1990–2019: 3.91–4.87 mm/year.

Coral Reefs and Vulnerability

  • Sunlight dependency: Rise in sea level reduces light penetration ? coral bleaching.
  • Stress factors: Ocean warming, acidification, changing tides, and coastal erosion.
  • Coral bleaching linked to El Niño and negative Indian Ocean Dipole (IOD)

Use of Coral Microatolls in Research

  • Definition: Disk-shaped coral colonies growing sideways when vertical growth is restricted by tide levels.
  • Serve as natural recorders of sea-level variations.
  • Research method: Uranium-thorium dating + growth band analysis (like tree rings).
  • Advantage: Provide long-term, high-resolution sea-level records in tectonically stable areas.

Findings of the Study

  • Sea-level rise began decades earlier than tide-gauge records suggested.
  • Regional differences:
    • Central Indian Ocean: Earlier, stronger acceleration.
    • Coastal Indian Ocean: More recent acceleration.
  • Drivers: Oceanic and atmospheric changes (e.g., intensified Southern Hemisphere westerlies, increased ocean heat uptake, shifts in ITCZ).

Implications for Island Nations

  • Nations at risk: Maldives, Lakshadweep, Chagos archipelago.
  • Risks: Submergence of land, loss of biodiversity, damage to infrastructure, displacement of populations.
  • Importance of historical reconstruction: Enables better climate adaptation planning.

Way Forward:

  • Expand monitoring using coral microatolls across the Indian Ocean basin.
  • Enhance adaptation strategies for vulnerable island nations through coastal protection and relocation planning.
  • Strengthen international cooperation on climate finance and technology transfer for resilience building.
  • Integrate regional sea-level histories into IPCC models for improved projections.

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