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Alan Robock Department of Environmental Sciences Rutgers University, New Brunswick, New Jersey USA

Lecture 11, 10/14/13. Climate Dynamics 11:670:461. Alan Robock Department of Environmental Sciences Rutgers University, New Brunswick, New Jersey USA. robock@envsci.rutgers.edu. http://envsci.rutgers.edu/~ robock. A thermally direct circulation. Fig. 7.1.

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Alan Robock Department of Environmental Sciences Rutgers University, New Brunswick, New Jersey USA

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  1. Lecture 11, 10/14/13 Climate Dynamics11:670:461 Alan Robock Department of Environmental Sciences Rutgers University, New Brunswick, New Jersey USA robock@envsci.rutgers.edu http://envsci.rutgers.edu/~robock

  2. A thermally direct circulation Fig. 7.1

  3. Annual mean, zonal mean meridional (m/s) and vertical velocities (interval 5 x 10-3 Pa/s) Fig. 7.2

  4. Zonal mean stream function (x 1010 kg/s), positive is clockwise. Fig. 7.3

  5. http://www.physicalgeography.net/fundamentals/7p.html

  6. http://www.physicalgeography.net/fundamentals/7p.html

  7. http://www.geogonline.org.uk/g3a_ki2.1.htm

  8. http://www.personal.psu.edu/czn115/blogs/meteo241/2010/10/e-portfolio-2.htmlhttp://www.personal.psu.edu/czn115/blogs/meteo241/2010/10/e-portfolio-2.html

  9. Surface currents relative to surface winds. Fig. 8.1

  10. Ekman spiral in the Northern Hemisphere Fig. 8.2

  11. Atlantic, 34.5ºN Depth (m) Percent oxygen saturation (lower values = older water) Pacific, 180ºW Depth (m) Fig. 8.4

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