Limiting global warming to 2 °C is unlikely to save most coral reefs
Author(s) -
Katja Frieler,
Malte Meinshausen,
Antonius Golly,
Matthias Mengel,
K. Lebek,
Simon D. Donner,
Ove HoeghGuldberg
Publication year - 2012
Publication title -
nature climate change
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 6.749
H-Index - 189
eISSN - 1758-6798
pISSN - 1758-678X
DOI - 10.1038/nclimate1674
Subject(s) - coral bleaching , environmental science , coral reef , reef , coral , global warming , ocean acidification , limiting , effects of global warming on oceans , climate change , sea surface temperature , ecosystem , resilience of coral reefs , range (aeronautics) , oceanography , representative concentration pathways , climatology , atmospheric sciences , ecology , climate model , geology , biology , engineering , materials science , composite material , mechanical engineering
Mass coral bleaching events have become a widespread phenomenon causing serious concerns with regard to the survival of corals. Triggered by high ocean temperatures, bleaching events are projected to increase in frequency and intensity. Here, we provide a comprehensive global study of coral bleaching in terms of global mean temperature change, based on an extended set of emissions scenarios and models. We show that preserving >10% of coral reefs worldwide would require limiting warming to below 1.5 °C (atmosphere–ocean general circulation models (AOGCMs) range: 1.3–1.8 °C) relative to pre-industrial levels. Even under optimistic assumptions regarding corals’ thermal adaptation, one-third (9–60%, 68% uncertainty range) of the world’s coral reefs are projected to be subject to long-term degradation under the most optimistic new IPCC emissions scenario, RCP3-PD. Under RCP4.5 this fraction increases to two-thirds (30–88%, 68% uncertainty range). Possible effects of ocean acidification reducing thermal tolerance are assessed within a sensitivity experiment. Download references
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