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Card 1a. Discrete Ordinate Multiple Scattering Algorithm: Issacs Two-Stream Algorithm (fast but less accurate) Multiple Scattering Algorithm.

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Presentation on theme: "Card 1a. Discrete Ordinate Multiple Scattering Algorithm: Issacs Two-Stream Algorithm (fast but less accurate) Multiple Scattering Algorithm."— Presentation transcript:

1 Card 1a

2 Discrete Ordinate Multiple Scattering Algorithm: Issacs Two-Stream Algorithm (fast but less accurate) Multiple Scattering Algorithm

3 Number of Streams to be used by DISORT – the higher the number the longer the run time 8 is a recommended value for most applications

4 Option to read solar irradiances from a file: Use default spectral solar irradiances Read from file (requires ISUN input)

5 Full Width Half Max FWHM of the triangular scanning function used to smooth the top of the atmosphere (TOA) solar irradiances (wavenumbers)

6 CO 2 mixing ratio in ppmv: Inputs of zero or leaving it blank defaults to an input of 330 ppmv Recommended value is closer to 365 ppmv

7 Vertical Water Vapor Column: If blank or zero the default is used If a leading character of “g” is used before the number the units will be in g/cm 2 (e.g., g 2 ) If a leading character of “a” is used the before the number the units will be in atm-cm Otherwise a numerical input will be considered a scaling factor applied to default water vapor column

8 Vertical Ozone Column: If blank or zero the default is used If a leading character of “g” is used before the number the units will be in g/cm 2 (e.g., g 2 ) If a leading character of “a” is used the before the number the units will be in atm-cm

9 Solar Radiance Data File Option: Use Default Solar Radiance File Read in a Solar Radiance File

10 Band Model Option: Use Default Band Model Read in Band Model File

11 Instrument Filter Option: Use Default Filter Read in Instrument Function File

12 TOA Solar Irradiance Scale Factor


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