Kalmus P, Ekanayaka A, Kang E, Baird M, Gierach M
Jet Propulsion Laboratory California Institute of Technology Pasadena CA USA.
University of Cincinnati Cincinnati OH USA.
Earths Future. 2022 May;10(5):e2021EF002608. doi: 10.1029/2021EF002608. Epub 2022 May 5.
Coral reefs are rapidly declining due to local environmental degradation and global climate change. In particular, corals are vulnerable to ocean heating. Anomalously hot sea surface temperatures (SSTs) create conditions for severe bleaching or direct thermal death. We use SST observations and CMIP6 model SST to project thermal conditions at reef locations at a resolution of 1 km, a 16-fold improvement over prior studies, under four climate emissions scenarios. We use a novel statistical downscaling method which is significantly more skillful than the standard method, especially at near-coastal pixels where many reefs are found. For each location we present projections of thermal departure (TD, the date after which a location with steadily increasing heat exceeds a given thermal metric) for severe bleaching recurs every 5 years (TD5Y) and every 10 years (TD10Y), accounting for a range of post-bleaching reef recovery/degradation. As of 2021, we find that over 91% and 79% of 1 km reefs have exceeded TD10Y and TD5Y, respectively, suggesting that widespread long-term coral degradation is no longer avoidable. We project 99% of 1 km reefs to exceed TD5Y by 2034, 2036, and 2040 under SSP5-8.5, SSP3-7.0, and SSP2-4.5 respectively. We project that 2%-5% of reef locations remain below TD5Y at 1.5°C of mean global heating, but 0% remain at 2.0°C. These results demonstrate the importance of further improving ecological projection capacity for climate-vulnerable marine and terrestrial species and ecosystems, including identifying refugia and guiding conservation efforts. Ultimately, saving coral reefs will require rapidly reducing and eliminating greenhouse gas emissions.
由于当地环境退化和全球气候变化,珊瑚礁正在迅速衰退。特别是,珊瑚很容易受到海洋升温的影响。异常炎热的海面温度(SST)为严重白化或直接热死亡创造了条件。我们利用SST观测数据和CMIP6模型SST,在四种气候排放情景下,以1公里的分辨率预测珊瑚礁位置的热状况,这比之前的研究提高了16倍。我们使用了一种新颖的统计降尺度方法,该方法比标准方法的技能显著更高,尤其是在发现许多珊瑚礁的近岸像素处。对于每个位置,我们给出了热偏差(TD,即热量持续增加的位置超过给定热指标的日期)的预测,严重白化每5年(TD5Y)和每10年(TD10Y)出现一次,同时考虑了白化后珊瑚礁恢复/退化的范围。截至2021年,我们发现超过91%和79%的1公里珊瑚礁分别超过了TD10Y和TD5Y,这表明广泛的长期珊瑚退化已无法避免。在SSP5-8.5、SSP3-7.0和SSP2-4.5情景下,我们预测到2034年、2036年和2040年,99%的1公里珊瑚礁将超过TD5Y。我们预测,在全球平均升温1.5°C时,2%-5%的珊瑚礁位置仍低于TD5Y,但在升温2.0°C时则没有。这些结果表明,进一步提高对气候脆弱的海洋和陆地物种及生态系统的生态预测能力非常重要,包括确定避难所和指导保护工作。最终,拯救珊瑚礁将需要迅速减少和消除温室气体排放。