Ocean Successive Orders with Atmosphere - Advanced (OSOAA) : Accurate computation of the radiative tranfer into the Ocean-Atmosphere system including polarisation, coupling terms, and the agitated surface.
How can I guarantee the OSOAA model assimilates the external Mueller Matrix?
To understand how the geometry of acquisition can affect remote sensing reflectance and polarimetry, I try to run OSOAA using an external file Mueller Matrix:
How can I guarantee the OSOAA model assimilates the external Mueller Matrix?
To understand how the geometry of acquisition can affect remote sensing reflectance and polarimetry, I try to run OSOAA using an external file Mueller Matrix:
EXTINCTION_COEF : 0.847090 SCATTERING_COEF : 3.056208 NB_LINES : 198 Angle F11 -F12/F11 F22/F11 F33/F11 0.01 91294.653 0.000001 1.000000 1.000000 0.02 75593.203 0.000003 1.000000 1.000000 ... 177.00 0.002 0.006599 0.979382 -0.977182 178.00 0.002 0.004895 0.978440 -0.975687 179.00 0.002 0.004470 0.978497 -0.972175
I selected the option "-HYD.Model 2", however, it seems the model keeps running option 1 because the "Main.log" indicates "HYD.Model: 1".
HYDROSOLS RADIATIVE PROPERTIES COMPUTATION
=> Characterization by models for PHYTOPLANKTON :
--> OSOAA_HYDROSOLS is called with the parameters : FICANGLES_RES_MIE : /local/OSOAA_RESULTS/0.517/Advanced_outputs/MIE_UsedAngles.txt
Simulation wavelength (Wa) : 0.51700 IMOD_HYD : 1 Concentration : 0.00000
=> Characterization by models for MINERAL-LIKE PARTICLES :
--> OSOAA_HYDROSOLS is called with the parameters : FICANGLES_RES_MIE : /local/OAA_RESULTS/0.517/Advanced_outputs/MIE_UsedAngles.txt
Simulation wavelength (Wa) : 0.51700 IMOD_HYD : 1 Concentration : 0.00000