Timescales for detection of trends in the ocean carbon sink

被引:0
|
作者
Galen A. McKinley
Darren J. Pilcher
Amanda R. Fay
Keith Lindsay
Matthew C. Long
Nicole S. Lovenduski
机构
[1] University of Wisconsin—Madison,Department of Atmospheric and Oceanic Sciences
[2] Center for Climatic Research,Department of Atmospheric and Oceanic Sciences and Institute of Arctic and Alpine Research
[3] University of Wisconsin—Madison,undefined
[4] Madison,undefined
[5] Space Science and Engineering Center,undefined
[6] University of Wisconsin—Madison,undefined
[7] NOAA Pacific Marine Environmental Laboratory,undefined
[8] National Center for Atmospheric Research,undefined
[9] University of Colorado Boulder,undefined
来源
Nature | 2016年 / 530卷
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摘要
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 then, internal climate variability will preclude such detection.
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页码:469 / 472
页数:3
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