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Past the Precipice? Projected Coral Habitability Under Global Heating

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...

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Autores principales: Kalmus, P., Ekanayaka, A., Kang, E., Baird, M., Gierach, M.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley and Sons Inc. 2022
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9287014/
https://www.ncbi.nlm.nih.gov/pubmed/35865222
http://dx.doi.org/10.1029/2021EF002608
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author Kalmus, P.
Ekanayaka, A.
Kang, E.
Baird, M.
Gierach, M.
author_facet Kalmus, P.
Ekanayaka, A.
Kang, E.
Baird, M.
Gierach, M.
author_sort Kalmus, P.
collection PubMed
description 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(2) reefs have exceeded TD10Y and TD5Y, respectively, suggesting that widespread long‐term coral degradation is no longer avoidable. We project 99% of 1 km(2) 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.
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spelling pubmed-92870142022-07-19 Past the Precipice? Projected Coral Habitability Under Global Heating Kalmus, P. Ekanayaka, A. Kang, E. Baird, M. Gierach, M. Earths Future Research Article 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(2) reefs have exceeded TD10Y and TD5Y, respectively, suggesting that widespread long‐term coral degradation is no longer avoidable. We project 99% of 1 km(2) 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. John Wiley and Sons Inc. 2022-05-05 2022-05 /pmc/articles/PMC9287014/ /pubmed/35865222 http://dx.doi.org/10.1029/2021EF002608 Text en © 2022. Commonwealth of Australia and Jet Propulsion Laboratory. California Institute of Technology. Government sponsorship acknowledged. https://creativecommons.org/licenses/by-nc/4.0/This is an open access article under the terms of the http://creativecommons.org/licenses/by-nc/4.0/ (https://creativecommons.org/licenses/by-nc/4.0/) License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited and is not used for commercial purposes.
spellingShingle Research Article
Kalmus, P.
Ekanayaka, A.
Kang, E.
Baird, M.
Gierach, M.
Past the Precipice? Projected Coral Habitability Under Global Heating
title Past the Precipice? Projected Coral Habitability Under Global Heating
title_full Past the Precipice? Projected Coral Habitability Under Global Heating
title_fullStr Past the Precipice? Projected Coral Habitability Under Global Heating
title_full_unstemmed Past the Precipice? Projected Coral Habitability Under Global Heating
title_short Past the Precipice? Projected Coral Habitability Under Global Heating
title_sort past the precipice? projected coral habitability under global heating
topic Research Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9287014/
https://www.ncbi.nlm.nih.gov/pubmed/35865222
http://dx.doi.org/10.1029/2021EF002608
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