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Published byAllen Ward Modified over 9 years ago
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E = o T 4
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Variables ListPower = Irradiance * Area
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Variables List mass = (2897 m K)/T
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E (at latitude a) = (1378.5 W m -2 )(sin a)
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Albedo = (Upwelling) / (Downwelling radiaiton) ? ? ? ? ? ? ? ? ? ? ? ?
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Figure 8 - Infrared Water Vapor Imagery for 11 March 2000 at 1745 UTC (11:45 AM CST)
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Figure 9 - Visible Satellite Imagery for 11 March 2000 at 1745 UTC (11:45 AM CST) Figure 8 - Infrared Water Vapor Imagery for 11 March 2000 at 1745 UTC (11:45 AM CST)
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Figure 8 - Infrared Water Vapor Imagery for 11 March 2000 at 1745 UTC (11:45 AM CST) Figure 12 - Incoming Solar Radiation (in W m-2) for 11 March 2000 at 11:30 AM CST (1730 UTC), as Measured by the Oklahoma Mesonet Figure 13 - Incoming Solar Radiation (in W m-2) for 11 March 2000 at 11:30 AM CST (1730 UTC), as Measured by the Oklahoma Mesonet
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Figure 9 - Visible Satellite Imagery for 11 March 2000 at 1745 UTC (11:45 AM CST) Figure 8 - Infrared Water Vapor Imagery for 11 March 2000 at 1745 UTC (11:45 AM CST)
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Figure 9 - Visible Satellite Imagery for 11 March 2000 at 1745 UTC (11:45 AM CST) Figure 8 - Infrared Water Vapor Imagery for 11 March 2000 at 1745 UTC (11:45 AM CST)
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Figure 8 - Infrared Water Vapor Imagery for 11 March 2000 at 1745 UTC (11:45 AM CST)
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Figure 9 - Visible Satellite Imagery for 11 March 2000 at 1745 UTC (11:45 AM CST)
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Figure 12 - Incoming Solar Radiation (in W m-2) for 11 March 2000 at 11:30 AM CST (1730 UTC), as Measured by the Oklahoma Mesonet
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Figure 13 - Incoming Solar Radiation (in W m-2) for 11 March 2000 at 11:30 AM CST (1730 UTC), as Measured by the Oklahoma Mesonet
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