July 25, 2025
What is Marine Heatwaves? UPSC
Why in News? A major 24-year-long coral reef monitoring study in the Lakshadweep archipelago, conducted by the Nature Conservation Foundation, has revealed a significant 50% decline in coral cover since 1998 due to repeated marine heatwaves driven by climate change.
Key Points:
- Study Details:
- Published in the journal Diversity and Distributions.
- Title: “Local Environmental Filtering and Frequency of Marine Heatwaves Influence Decadal Trends in Coral Composition”.
- Based on long-term monitoring (1998–2022) of coral reefs at Agatti, Kadmat, and Kavaratti atolls in Lakshadweep.
- Key Findings:
- Coral cover declined from 37.24% in 1998 to 19.6% in 2022.
- Represents a ~50% decline in coral reef health over 24 years.
- Causes:
- Repeated marine heatwaves due to El Niño Southern Oscillation (ENSO) events in 1998, 2010, and 2016.
- Intensified by global climate change.
- Recovery Patterns:
- Reduced recovery rates after each bleaching event, though coral mortality decreased with successive events.
- Critical recovery period identified: At least six years of bleaching-free conditions are needed for significant coral regeneration.
- Local Factors Matter:
- Recovery varies depending on wave exposure, depth, and other site-specific environmental filters.
- Predictive Framework:
- Study offers a predictive model to identify vulnerable vs. resilient reefs, aiding in conservation planning.
About Marine Heatwaves:
Definition:
Marine heatwaves (MHWs) are prolonged periods of unusually high sea surface temperatures (SSTs) in a particular ocean region. These events typically last for days to months and can extend over hundreds to thousands of kilometers.
Key Features of Marine Heatwaves:
Feature |
Details |
Temperature Threshold |
SST above the 90th percentile of historical averages (for that time of year) |
Duration |
At least 5 consecutive days or more |
Causes |
Ocean warming due to climate change, ENSO events, reduced ocean mixing, changes in currents |
Measurement |
Tracked using satellite SST data and in-situ observations |
Causes of Marine Heatwaves:
- Climate Change:
- Increases global ocean temperatures, making heatwaves more frequent and intense.
- Atmospheric Blocking & High-Pressure Systems:
- Trap heat near the ocean surface and reduce cooling.
- El Niño Events:
- Trigger large-scale warming in the Pacific, influencing global marine heatwaves.
- Reduced Ocean Mixing:
- Less vertical movement of cold water weakens natural ocean cooling.
Impacts of Marine Heatwaves:
Sector |
Impact |
Coral Reefs |
Mass bleaching, death of corals (e.g., Lakshadweep, Great Barrier Reef) |
Marine Biodiversity |
Fish migration, plankton decline, loss of breeding grounds |
Fisheries |
Decline in fish stocks, affecting coastal economies |
Ocean Health |
Disruption of food chains, ecosystem imbalance |
Weather Patterns |
May influence cyclone formation and rainfall patterns |
Examples of Marine Heatwaves:
- Lakshadweep Archipelago: Repeated heatwaves since 1998 caused ~50% coral decline.
- The Blob (2013–2016): A massive Pacific Ocean marine heatwave causing widespread ecological disruption.
- Great Barrier Reef (Australia): Severely bleached during marine heatwaves in 2016, 2017, and 2020.
Possible Solutions / Way Forward:
- Global climate action to reduce greenhouse gas emissions.
- Marine Protected Areas (MPAs) to reduce local stressors.
- Coral restoration projects using heat-resistant species.
- Early warning systems using satellite and ocean data.
- Strengthening local governance and community-based adaptation.