Extended warming of the northern high latitudes due to an overshoot of the Atlantic meridional overturning circulation
Article first published online: 20 DEC 2011
© 2011 by the American Geophysical Union
Geophysical Research Letters
Volume 38, Issue 24, 28 December 2011
How to Cite
2011), Extended warming of the northern high latitudes due to an overshoot of the Atlantic meridional overturning circulation, Geophys. Res. Lett., 38, L24704, doi:10.1029/2011GL049998., , , and (
- Issue published online: 20 DEC 2011
- Article first published online: 20 DEC 2011
- Manuscript Revised: 10 NOV 2011
- Manuscript Accepted: 10 NOV 2011
- Manuscript Received: 13 OCT 2011
Auxiliary material for this article contains a figure showing the AMOC trajectories as a function of CO2 concentrations and an animation showing the evolution of zonal mean salinity cross section in the Arctic-Atlantic sector.
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|grl28778-sup-0001-readme.txt||plain text document||1K||readme.txt|
|grl28778-sup-0002-fs01.eps||PS document||530K||Figure S1. AMOC trajectories as function of atmospheric CO2 concentrations in three HadCM3 experiments as shown by the different colours.|
|grl28778-sup-0003-ms01.gif||GIF image||9099K||Animation S1. The build-up of the north-south salinity gradient under global warming and the subsequent release of the subtropical salty water pool following climate mitigation action.|
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