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Project A10 – Scientific questions and results

 

To what extent do changes in Atlantic meridional overturning circulation control global thermocline depth during the Pliocene (a potential analogue for the near future) and the late Pleistocene (including glacial shutdown of deep-water production)?

Early Pliocene shoaling of the East Pacific tropical thermocline

Which role does upper ocean stratification play in amplifying/reducing atmospheric-oceanic heat and gas exchange during “Greenhouse” and “Icehouse” climate scenarios?

 

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Impressum | © marum | Diese Seite wurde zuletzt aktualisiert von: Dr. Frank Schmieder. Datum: 05.11.2009, 15:45 Uhr