Estimating the Atlantic overturning at 26N using satellite altimetry [IUGG]
Thermohaline circulation ●The concept of meridional overturning ●Deep water formation and property Antarctic Bottom Water North Atlantic Deep Water Antarctic.
18 April 2007 Climate Change 2007: The Physical Science Basis Chapter 5:Observations: Oceanic Climate Change and Sea Level The Working Group I Report of.
THOR Annual Meeting Paris, 24 November 2009 Nuno Nunes, Jürgen Fischer,Rainer Zantopp, Martin Visbeck Recent changes in properties and transport in the.
Oceanography & Climate Synthesis Question: If all of the oceans currents changed direction, would they then heat the equator and cool the poles?
Thermohaline circulation ●The meridional overturning ●Deep water formation and property Antarctic Bottom Water North Atlantic Deep Water Antarctic Intermediate.
Nathan Bindoff and lead authors ACECRC, IASOS, CSIRO MAR University of Tasmania TPAC
Lecture 5 The Climate System and the Biosphere. One significant way the ocean can influence climate is through formation of sea ice. Sea ice is much more.
Www.csiro.au Seeing under the ice: a strategy for observing the Southern Ocean beneath sea ice and ice shelves Steve Rintoul CSIRO Marine and Atmospheric.
Ocean Current Switching: Can changes in ocean circulation cause rapid climate change? Richard Karsten Department of Mathematics and Statistics [email protected].
01 March 2007Royal Society Meeting Climate Change 2007: The Physical Science Basis Chapter 5:Observations: Oceanic Climate Change and Sea Level The Working.
Direct measurement of the deep circulation within the Brazil Basin