大西洋珊瑚礁增长减缓超过2°C,海平面的影响会加大
Chris T Perry1, Didier M de Bakker2, Alice E Webb2
1Geography, Faculty of Environment, Science and Economy, University of Exeter, Exeter, UK. c.perry@exeter.ac.uk.
Nature
|September 17, 2025
概括
珊瑚礁因气候变化而受到侵蚀, 即使恢复,海平面上升的影响预计在2100年没有积极的气候缓解.
科学领域:
- 海洋生物学
- 气候科学
- 沿海地质
背景情况:
- 珊瑚礁提供自然海岸防洪.
- 气候变化,海平面上升和局部压力因素影响了珊瑚礁的生长.
- 预计在珊瑚礁上方水深的增加不太清楚,这限制了沿海脆弱性的评估.
研究的目的:
- 分析珊瑚礁的化石沉积物, 以将珊瑚礁生态与生长潜力联系起来.
- 在不同的气候场景下,评估到2100年珊瑚礁上方水深的预测增长.
- 评估这些变化对沿海洪水风险的影响.
主要方法:
- 分析来自400多个热带大西洋地区的珊瑚礁化石.
- 模拟各种共享社会经济路径 (SSP) 的珊瑚礁增长潜力和海平面上升.
- 预测到2100年珊瑚礁表面的水深变化.
主要成果:
- 到2040年,超过70%的珊瑚礁可能会被侵蚀.
- 如果全球变暖超过2°C, 至少99%的珊瑚礁将在2100年被侵蚀.
- 预计到2100年水深将增加0.7-1.2米,
结论:
- 珊瑚礁生长和SLR的不同轨迹将大大增加沿海洪水的风险.
- 珊瑚礁的恢复可以部分减轻SLR的影响, 但需要积极的气候减缓.
- 迫切需要采取气候行动来保护珊瑚礁功能并减少沿海的脆弱性.
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