Williamson, P, Turley, CM and Ostle, C 2017 Ocean acidification. MCCIP. (UNSPECIFIED)
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Williamson et al 2017 MCCIP OA.pdf - Published Version Available under License Open Government Licence. Download (1MB) | Preview |
Abstract/Summary
KEY HEADLINES • Global-scale patterns and processes of ocean acidification are superimposed on other factors influencing seawater chemistry over local to regional space scales, and hourly to seasonal time scales. • Future ocean conditions will depend on future CO2 emissions; there is now international agreement that these should be reduced to net zero, thereby reducing the consequences of both climate change and ocean acidification. • Assessments of ocean acidification by the Intergovernmental Panel on Climate Change (IPCC) gave high or very high confidence to chemical aspects, but a much wider range of confidence levels to projected biological and biogeochemical impacts. Biotic impacts will depend on species-specific responses, interactions with other stressors and food-web effects. • Previous MCCIP statements are considered to still be valid, with increased confidence for some aspects. • Observed pH decreases in the North Sea (over 30 years) and at coastal UK sites (over 6 years) seem more rapid than in the North Atlantic as a whole. However, shelf sea and coastal data sets show high variability over a range of timescales, and factors affecting that variability need to be much better understood. • UK research on ocean acidification has been productive and influential. There is no shortage of important and interesting topic areas that would improve scientific knowledge and deliver societally-important outcomes.
Item Type: | Publication - Report (UNSPECIFIED) |
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Subjects: | Earth Sciences Ecology and Environment Fisheries Marine Sciences |
Divisions: | Plymouth Marine Laboratory > Science Areas > Sea and Society |
Depositing User: | Dr Carol Turley |
Date made live: | 27 Apr 2018 10:32 |
Last Modified: | 22 Aug 2018 15:02 |
URI: | https://plymsea.ac.uk/id/eprint/7781 |
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