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Alan Robock Department of Environmental Sciences

Lecture 9, 10/3/13. 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. Fig. 5.3.

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Alan Robock Department of Environmental Sciences

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  1. Lecture 9, 10/3/13 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. Fig. 5.3

  3. Climatological annual mean energy budget for 2000–2005 (W/m2). (Trenberth & Fasullo, 2011) https://climatedataguide.ucar.edu/climate-data/budgets-mass-moisture-energy

  4. Global, annual average heat balance (W/m2) Fig. 5.4

  5. Planetary albedo (a) is the average reflectivity of the Earth = 102/341 = 0.30 Climatological annual mean energy budget for 2000–2005 (W/m2). (Trenberth & Fasullo, 2011) https://climatedataguide.ucar.edu/climate-data/budgets-mass-moisture-energy

  6. Outer Space: Total = 341 W m‑2– (239 + 102) W m‑2 = 0 W m‑2 Climatological annual mean energy budget for 2000–2005 (W/m2). (Trenberth & Fasullo, 2011) https://climatedataguide.ucar.edu/climate-data/budgets-mass-moisture-energy

  7. Outer Space: Total = 341.3 W m‑2– (238.5 + 101.9) W m‑2 = -0.9 W m‑2 Climatological annual mean energy budget for 2000–2005 (W/m2). (Trenberth & Fasullo, 2011) https://climatedataguide.ucar.edu/climate-data/budgets-mass-moisture-energy

  8. Atmosphere: Total = (78 + 17 + 80 + 374) W m‑2 - (187 + 30 + 333) W m‑2 = -1 W m‑2 Climatological annual mean energy budget for 2000–2005 (W/m2). (Trenberth & Fasullo, 2011) https://climatedataguide.ucar.edu/climate-data/budgets-mass-moisture-energy

  9. T = 255 K T = 288 K Greenhouse effect Surface: Total = (161 + 333) W m‑2 - (17 + 80 + 396) W m‑2 = 1 W m‑2 Climatological annual mean energy budget for 2000–2005 (W/m2). (Trenberth & Fasullo, 2011) https://climatedataguide.ucar.edu/climate-data/budgets-mass-moisture-energy

  10. Annual average incident solar radiation (W/m2) Annual average absorbed solar radiation at top of atmosphere (W/m2) Fig. 5.5

  11. Planetary albedo (%) Fig. 5.6

  12. Dependence of water albedo on solar zenith angle, θZ Fig. 5.7

  13. Annual mean outgoing longwave radiation (W/m2) Fig. 5.8

  14. Net radiation at top of atmosphere (W/m2) Fig. 5.9

  15. Net radiation at top of atmosphere (W/m2) Fig. 5.9

  16. Solar radiation absorbed at surface, SABS (W/m2) Fig. 5.10

  17. Outgoing longwave radiation at surface, esT4 (W/m2) Fig. 5.11a

  18. Downward back radiation at surface, FBACK (W/m2) Fig. 5.11b

  19. Sensible heat flux at surface, HS (W/m2) Fig. 5.12a

  20. Latent heat flux at surface, HL (W/m2) Fig. 5.12b

  21. Horizontal and vertical heat fluxes at surface, FH + FV (W/m2) Fig. 5.13

  22. A thermally direct circulation Fig. 7.1

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

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

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

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

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

  28. 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

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