Timescales for detection of trends in the ocean carbon sink

A climate modelling experiment is used to identify where ocean carbon uptake should change as a result of anthropogenic climate change and to distinguish these changes from internal climate variability; we may be able to detect changing uptake in some oceanic regions between 2020 and 2050, but until...

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Veröffentlicht in:	Nature (London) 2016-02, Vol.530 (7591), p.469-472
Hauptverfasser:	McKinley, Galen A., Pilcher, Darren J., Fay, Amanda R., Lindsay, Keith, Long, Matthew C., Lovenduski, Nicole S.
Format:	Artikel
Sprache:	eng
Schlagworte:	704/106/47 704/106/829/827 Anthropogenic factors Atmosphere - chemistry Carbon Cycle Carbon dioxide Carbon Dioxide - analysis Carbon Sequestration Carbon sinks Climate change Climate Change - statistics & numerical data Climate variability Ecosystem Environmental aspects Human Activities Humanities and Social Sciences letter Models, Theoretical multidisciplinary Observation Ocean Ocean circulation Oceans Oceans and Seas Science Seawater - chemistry Time Factors Time series Trends
Online-Zugang:	Volltext
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