Are These Islands Invincible to Sea Level Rise?
By PBS Terra
Key Concepts:
- Sea Level Rise (SLR)
- Atoll Islands: Ring-shaped islands formed atop coral reefs.
- Island Dynamics: The processes of sediment deposition and erosion that shape islands.
- Sediment Deposition: The accumulation of sand and other materials on islands, often during floods.
- Buffer Zones: Undeveloped coastal areas that allow for natural sediment deposition.
- Coral Bleaching: The loss of color in coral due to environmental stress, impacting sediment production.
- Adaptation Strategies: Methods for coastal communities to cope with SLR, including sea walls, relocation, and natural solutions.
1. The Paradox of Growing Atoll Islands
- Main Point: While sea level rise threatens low-lying atoll islands, some studies show that many of these islands are stable or even growing.
- Details: A 2018 study by Paul Kench analyzing Tuvalu's islands between 1971 and 2014 found that eight of nine atolls and almost three-fourths of the islands grew, increasing overall land area by 2.9%. Similar findings were reported in the Maldives, where more islands got bigger than smaller.
- Conflicting Experiences: Despite the data showing island growth, residents report experiencing the impacts of climate change in their daily lives.
2. Island Dynamics: Expansion vs. Elevation
- Lamese's Research: Lamese studied a small island on Funafuti, Tuvalu, using drone data to assess changes in circumference and volume.
- Findings: The island was expanding in circumference but losing volume, indicating a decrease in elevation.
- Explanation: Waves and currents deposit sand on one side of the island while eroding it from another, causing the island to spread out but not necessarily increase in height.
- Implications: While islands may appear to be growing, lower elevation increases vulnerability to flooding and sea level rise.
3. Traditional Adaptation Strategies and Their Limitations
- Sea Walls: A common solution, but expensive (millions to tens of millions of dollars per atoll island) and potentially unsustainable in the long run.
- Relocation: Moving entire populations from their ancestral lands is a drastic and undesirable solution.
- Quote: "Now I, I don't see either of these as viable solutions,"
4. The "Problem is the Solution" Hypothesis: Natural Sediment Deposition
- Core Idea: Flooding, the problem, is also the solution because it deposits sediment on islands, increasing their elevation.
- Process: Floodwaters carry sediment and deposit it on top of the island, building it up over time.
- Importance of Coral: This process relies on healthy coral reefs, which produce the sediment. Coral bleaching threatens this natural defense.
- Impact of Infrastructure: Human infrastructure like sea walls and roads can prevent sediment deposition, hindering natural island growth.
5. The Role of Buffer Zones and Natural Island States
- Buffer Zones: Undeveloped coastal areas that allow for natural sediment deposition.
- Recommendation: Maintain a vegetative buffer zone around islands, at least 25-30 meters wide.
- Natural State: Islands left in a relatively natural state are better able to move up and back with rising sea levels.
- Quote: "When we, we think the islands, if they're left as natural as possible, that they are able to move up and back with the rising sea level. So the islands will not drown. They will evolve."
6. The Importance of Storms and Floods
- Hurricanes: Churn up the ocean, carrying coral sand and sediment that piles on top of islands during landfall.
- Essential Role: Flooding from major storms is essential for island building and maintenance.
- Consequences of Prevention: Without flooding, many islands could disappear.
7. Applicability to Other Coastal Areas
- Limitations for Developed Cities: Cities like Miami and New York cannot accommodate flooding in the same way as atoll islands.
- Adaptable Environments: Sandy or gravelly coastal environments can adapt by allowing sediment to move naturally.
- Strategies: Avoiding critical infrastructure in vulnerable areas, moving infrastructure, and getting out of harm's way.
8. Long-Term Sea Level Rise and Adaptation
- Future Projections: Sea level rise will continue for some time, even beyond current projections to 2150.
- Historical Data: 125,000 years ago, with similar temperatures and CO2 levels, seas were 10-30 feet higher.
- Long-Term Changes: Significant sea level rise will require fundamental changes to our coastal footprint.
- Buying Time: Current adaptation strategies are primarily buying us time to adapt or relocate.
9. The Importance of Local Knowledge
- Critical Input: Adaptation strategies must consider the lived experiences of local communities.
- Ongoing Impacts: Communities are already experiencing the impacts of climate change.
- Quote: "It's not just like whether we appear or disappear in the next a hundred years, but like right now, as I'm speaking, we already experienced those impacts of climate change."
10. Conclusion
- Natural Forces: Hurricanes and floods have shaped ecosystems for millennia and play a critical role in island survival.
- Future Challenges: As seas rise and storms intensify, more cities will need to adapt to these realities.
- Creative Solutions: Cities around the world have learned to live with water in creative ways.
Synthesis/Conclusion:
The video explores the complex relationship between sea level rise and the survival of atoll islands. While some studies suggest that these islands are growing, this growth often involves a decrease in elevation, increasing vulnerability to flooding. Traditional adaptation strategies like sea walls and relocation have limitations. A more sustainable approach involves embracing natural processes, such as sediment deposition during floods, and maintaining buffer zones. While this approach may not be applicable to all coastal areas, it offers valuable insights for managing coastal environments in the face of rising seas. Ultimately, long-term adaptation will require significant changes to our coastal footprint and a consideration of local knowledge and experiences.
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