alan robock department of environmental sciences

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Alan Robock Department of Environmental Sciences Rutgers University, New Brunswick, New Jersey USA [email protected]. edu http://envsci.rutgers.edu/~ robock Climate Dynamics 11:670:461 Lecture 9, 10/3/13

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Lecture 9, 10/3/13. Climate Dynamics 11:670:461. Alan Robock Department of Environmental Sciences Rutgers University, New Brunswick, New Jersey USA. [email protected]. http://envsci.rutgers.edu/~ robock. Fig. 5.3. - PowerPoint PPT Presentation

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Page 1: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental Sciences

Rutgers University, New Brunswick, New Jersey USA

[email protected]

http://envsci.rutgers.edu/~robock

Climate Dynamics11:670:461

Lecture 9, 10/3/13

Page 2: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

SciencesFig. 5.3

Page 3: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

Sciences

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

Page 4: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

SciencesFig. 5.4

Global, annual average heat balance (W/m2)

Page 5: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

Sciences

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

Planetary albedo (a) is the average reflectivity of the Earth = 102/341 = 0.30

Page 6: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

Sciences

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

Outer Space:

Total = 341 W m‑2 – (239 + 102) W m‑2 = 0 W m‑2

Page 7: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

Sciences

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

Outer Space:

Total = 341.3 W m‑2 – (238.5 + 101.9) W m‑2 = -0.9 W m‑2

Page 8: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

Sciences

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

Atmosphere:

Total = (78 + 17 + 80 + 374) W m‑2 - (187 + 30 + 333) W m‑2 = -1 W m‑2

Page 9: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

Sciences

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

Surface:

Total = (161 + 333) W m‑2 - (17 + 80 + 396) W m‑2 = 1 W m‑2

Greenhouse effect

T = 255 K

T = 288 K

Page 10: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

SciencesFig. 5.5

Annual average incident solar

radiation (W/m2)

Annual average absorbed solar

radiationat top of atmosphere

(W/m2)

Page 11: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

SciencesFig. 5.6 Planetary albedo

(%)

Page 12: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

SciencesFig. 5.7

Dependence of water albedo on solar zenith angle, θZ

Page 13: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

Sciences

Annual mean outgoing longwave radiation (W/m2)

Fig. 5.8

Page 14: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

Sciences

Net radiation at top of atmosphere (W/m2)

Fig. 5.9

Page 15: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

Sciences

Net radiation at top of atmosphere (W/m2)

Fig. 5.9

Page 16: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

Sciences

Solar radiation absorbed at surface, SABS (W/m2)

Fig. 5.10

Page 17: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

Sciences

Outgoing longwave radiation at surface, esT4 (W/m2)

Fig. 5.11a

Page 18: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

Sciences

Downward back radiation at surface, FBACK (W/m2)

Fig. 5.11b

Page 19: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

Sciences

Sensible heat flux at surface, HS (W/m2)

Fig. 5.12a

Page 20: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

Sciences

Latent heat flux at surface, HL (W/m2)

Fig. 5.12b

Page 21: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

Sciences

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

Fig. 5.13

Page 22: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

SciencesFig. 7.1

A thermally direct circulation

Page 23: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

SciencesFig. 7.2

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

Page 24: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

SciencesFig. 7.3

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

Page 25: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

Sciences

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

Page 26: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

Sciences

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

Page 27: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

Sciences

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

Page 28: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

Sciences

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