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Climate Change Negotiations – UNFCCC, COP, Other Conventions and Protocols

Geoengineering Proposals for Polar Regions found flawed

Why in the News?

A University of Exeter study found five major polar geoengineering methods ineffective and risky, failing criteria for responsible climate intervention.

Geoengineering in Polar Regions: Study Findings

Method Description Intended Benefit Key Findings & Limitations
Stratospheric Aerosol Injection (SAI) Artificially releasing aerosols (SO₂, sulphur particles, TiO₂, CaCO₃) into the stratosphere to reflect sunlight. Reduce surface temperatures by blocking solar radiation.
  • Ineffective in polar winters (no sunlight) and of limited use in summers (ice already highly reflective).
  • Sudden termination can cause “termination shock” with rapid global warming.
  • Potential to disrupt global weather cycles, harming food and water security.
  • No global governance on costs or liability. Estimated cost: $55M/year per country (if 30 nations share).
Sea Curtains / Sea Walls Massive buoyant barriers anchored to seafloor to block warm currents from reaching ice sheets. Slow melting of glaciers by insulating them from warm water.
  • Technically near-impossible in remote seas like Amundsen (Antarctica).
  • Extremely high costs — >$1 billion/km.
  • Threatens marine circulation, fish migration, and nutrient cycles.
  • Installation in harsh polar seas only possible for few months a year; requires custom-built ships.
  • Risk of toxic materials leaching into ocean.
Sea Ice Management (Microbeads) Sprinkling glass microbeads over sea ice to increase albedo (reflectivity) and thicken ice. Preserve summer ice, slow down warming.
  • Requires 360M tonnes of beads annually — equal to world’s plastic production.
  • Major logistical and emissions challenges.
  • Beads dissolve quickly, reducing effectiveness.
  • Some studies show beads absorb sunlight, causing net warming.
  • Costly: $500B/year for Arctic deployment; requires 100M pumps, huge energy draw.
Basal Water Removal Pumping subglacial meltwater from under Antarctic glaciers. Reduce glacier sliding, thus slowing sea-level rise.
  • Flawed logic: subglacial water is constantly replenished by frictional/geothermal heating.
  • Highly emissions-intensive and energy-consuming.
  • Requires continuous monitoring, maintenance, and heavy infrastructure.
  • Long-term sustainability questioned.
Ocean Fertilisation Adding nutrients (e.g., iron) to stimulate phytoplankton growth, enhancing CO₂ absorption. Sequester more carbon in oceans.
  • No control over which phytoplankton species dominate, creating food chain imbalances. 
  • Could harm marine biodiversity and alter global nutrient cycles.
  • Needs deployment at massive, impractical scale.
  • Risk of side-effects outweighs uncertain benefits.

 

[UPSC 2020] Consider the following activities:

1. Spreading finely ground basalt rock extensively on farmlands

2. Increasing the alkalinity of oceans by adding lime

3. Capturing carbon dioxide released by various industries and pumping it into abandoned subterranean mines in the form of carbonated waters

How many of the above activities are often considered and discussed for carbon capture and sequestration?

Options: (a) Only one (b) Only two (c) All three* (d) None

 

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