Large‐scale ocean circulation‐cloud interactions reduce the pace of transient climate change

Changes to the large‐scale oceanic circulation are thought to slow the pace of transient climate change due, in part, to their influence on radiative feedbacks. Here we evaluate the interactions between CO2‐forced perturbations to the large‐scale ocean circulation and the radiative cloud feedback in...

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Veröffentlicht in:	Geophysical research letters 2016-04, Vol.43 (8), p.3935-3943
Hauptverfasser:	Trossman, D. S., Palter, J. B., Merlis, T. M., Huang, Y., Xia, Y.
Format:	Artikel
Sprache:	eng
Schlagworte:	Aerosol-cloud interactions Atmospheric models Brackish Carbon dioxide Circulation Climate Climate change Climate models Cloud-climate relationships Clouds Computer simulation Feedback feedbacks Global warming Heat Heat transport Interactions Loads (forces) Marine Meridional heat transport MOC Ocean circulation Ocean currents Ocean models Ocean temperature Ocean warming Perturbations Scale (ratio) transient Transport Transportation models Uncertainty Water circulation
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