Deep water flow speed and surface ocean changes in the subtropical North Atlantic during the last deglaciation

Climate fluctuations during the last deglaciation have been linked to changes in the North Atlantic Meridional Overturning Circulation (MOC) through its modulation of northward marine heat transport. Consequently, much research into the causes of rapid climate change has focused on the northern Nort...

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Veröffentlicht in:	Global and planetary change 2011-12, Vol.79 (3), p.255-263
Hauptverfasser:	Hall, I.R., Evans, H.K., Thornalley, D.J.R.
Format:	Artikel
Sprache:	eng
Schlagworte:	Circulation Climate change Deep water Deep Western Boundary Current Deglaciation Grain size Marine ocean circulation Oceans rapid climate change Southern Ocean Water depth
Online-Zugang:	Volltext
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