Single-scattering albedo of the soil particles. It characterizes the efficiency of an average particle to scatter and absorb light. One of the classical Hapke parameter.
This parameter gives the absolut lower limit of the single-scattering albedo of the soil particles. It characterizes the efficiency of an average particle to scatter and absorb light. If a sulution guess falls out-of-bonds then the attemp will be aborted and a new guess attempted.
This parameter gives the absolut upper limit of the single-scattering albedo of the soil particles. It characterizes the efficiency of an average particle to scatter and absorb light. If a sulution guess falls out-of-bonds then the attemp will be aborted and a new guess attempted.
This parameter gives temperatur for the single-scattering albedo of the soil
particles. It characterizes the efficiency of an average particle to scatter
and absorb light.
This parameter gives the range over which random guesses can be expected to
vary at first:
W_SOIL_NEW = T_W_SOIL * tan( PI * ran_num + PI/2 ).
As the system cools the range will constrict gradually :
T_W_SOIL_NEW_* = T_W_SOIL_OLD_* * scale,
scale depends of NUMTEN.
One of the classical Hapke parameter. Parameter which characterizes the soil structure in the terms of porosity, particle-size distribution, and rate of compaction with depth (angular width of opposition surge due to shadowing).
This parameter gives the absolut lower limit of the parameter which characterizes the soil structure (angular width of the opposition surge due to shadowing). If a sulution guess falls out-of-bonds then the attemp will be aborted and a new guess attempted.
This parameter gives the absolut upper limit of the parameter which characterizes the soil structure (angular width of the opposition surge due to shadowing). If a sulution guess falls out-of-bonds then the attemp will be aborted and a new guess attempted.
This parameter gives temperatur for the parameter which characterizes the soil
structure (angular width of the opposition surge due to shadowing).
This parameter gives the range over which random guesses can be expected to
vary at first:
H_SHOE_NEW = T_H_SHOE * tan( PI * ran_num + PI/2 ).
As the system cools the range will constrict gradually :
T_H_SHOE_NEW_* = T_H_SHOE_OLD_* * scale,
scale depends of NUMTEN.
One of the classical Hapke parameter. Opposition magnitude coefficient. The total amplitude of the opposition surge due to shadowing. It is the ratio of the light scattered from near the illuminated surface of the particle to the total amount of light scattered at zero phase : B_SHOE=S(0)/(W_SOIL*p(0)) with p(0) - soil phase function S(0) - opposition surge amplitude term which characterizes the contribution of light scattered from near the front surface of individual particles at zero phase. For a true, shadow-hiding opposition effect, 0<=B_SHOE<=1. However, there are several other phenomena that may also cause a surge in brightness at small phase angles. These including the following: 1) The coherent backscatter or weak photon localisation due to multiply scattered light. 2) An single-particle opposition effect caused by complex porous agglomerates ( soil phase function ) 3) Glory caused by sperical particles ( soil phase function ) 4) Internal reflections of transparent particles ( soil phase function ) These various phenomena may be large enough to increase the opposition surge by more than a factor of 2. This possibility may be taken into account by allowing B_SHOE to be greater than 1.
This parameter gives the absolut lower limit of the parameter which characterizes the opposition magnitude coefficient. If a sulution guess falls out-of-bonds then the attemp will be aborted and a new guess attempted.
This parameter gives the absolut upper limit of the parameter which characterizes theopposition magnitude coefficient. If a sulution guess falls out-of-bonds then the attemp will be aborted and a new guess attempted.
This parameter gives temperatur for the parameter which characterizes the
opposition magnitude coefficient.
This parameter gives the range over which random guesses can be expected to
vary at first:
B_SHOE_NEW = T_B_SHOE * tan( PI * ran_num + PI/2 ).
As the system cools the range will constrict gradually :
T_B_SHOE_NEW_* = T_B_SHOE_OLD_* * scale,
scale depends of NUMTEN.
Average topographic slope angle of surface roughness at subresolution scale. One of the classical Hapke parameter.
This parameter gives the absolut lower limit of the average topographic slope angle of surface roughness at subresolution scale. If a sulution guess falls out-of-bonds then the attemp will be aborted and a new guess attempted.
This parameter gives the absolut upper limit of the average topographic slope angle of surface roughness at subresolution scale. If a sulution guess falls out-of-bonds then the attemp will be aborted and a new guess attempted.
This parameter gives temperatur for the average topographic slope angle of
surface roughness at subresolution scale.
This parameter gives the range over which random guesses can be expected to
vary at first:
THETA_NEW = T_THETA * tan( PI * ran_num + PI/2 ).
As the system cools the range will constrict gradually :
T_THETA_NEW_* = T_THETA_OLD_* * scale,
scale depends of NUMTEN.
Parameter of the first term of the Henyey-Greenstein soil particle phase function. One of the classical Hapke parameter.
This parameter gives the absolut lower limit of the parameter of the first term of the Henyey-Greenstein soil particle phase function. If a sulution guess falls out-of-bonds then the attemp will be aborted and a new guess attempted.
This parameter gives the absolut upper limit of the parameter of the first term of the Henyey-Greenstein soil particle phase function. If a sulution guess falls out-of-bonds then the attemp will be aborted and a new guess attempted.
This parameter gives temperatur for the parameter of the first term of the
Henyey-Greenstein soil particle phase function.
This parameter gives the range over which random guesses can be expected to
vary at first:
HG1_SOIL_NEW = T_HG1_SOIL * tan( PI * ran_num + PI/2 ).
As the system cools the range will constrict gradually :
T_HG1_SOIL_NEW_* = T_HG1_SOIL_OLD_* * scale,
scale depends of NUMTEN.
Single scattering albedo of the atmospheric aerosols.
This parameter gives the absolut lower limit of the single scattering albedo of the atmospheric aerosols. If a sulution guess falls out-of-bonds then the attemp will be aborted and a new guess attempted.
This parameter gives the absolut upper limit of the single scattering albedo of the atmospheric aerosols. If a sulution guess falls out-of-bonds then the attemp will be aborted and a new guess attempted.
This parameter gives temperatur for the single scattering albedo of the
atmospheric aerosols.
This parameter gives the range over which random guesses can be expected to
vary at first:
W_ATM_NEW = T_W_ATM * tan( PI * ran_num + PI/2 ).
As the system cools the range will constrict gradually :
T_W_ATM_NEW_* = T_W_ATM_OLD_* * scale,
scale depends of NUMTEN.
Optical depth of the atmosphere.
This parameter gives the absolut lower limit of the optical depth of the atmosphere. If a sulution guess falls out-of-bonds then the attemp will be aborted and a new guess attempted.
This parameter gives the absolut upper limit of the optical depth of the atmosphere. If a sulution guess falls out-of-bonds then the attemp will be aborted and a new guess attempted.
This parameter gives temperatur for the optical depth of the atmosphere.
This parameter gives the range over which random guesses can be expected to
vary at first:
TAU_ATM_NEW = T_TAU_ATM * tan( PI * ran_num + PI/2 ).
As the system cools the range will constrict gradually :
T_TAU_ATM_NEW_* = T_TAU_ATM_OLD_* * scale,
scale depends of NUMTEN.
Parameter of the first term of the Henyey-Greenstein atmospheric phase function.
This parameter gives the absolut lower limit of the parameter of the first term of the Henyey-Greenstein atmospheric phase function. If a sulution guess falls out-of-bonds then the attemp will be aborted and a new guess attempted.
This parameter gives the absolut upper limit of the parameter of the first term of the Henyey-Greenstein atmospheric phase function. If a sulution guess falls out-of-bonds then the attemp will be aborted and a new guess attempted.
This parameter gives temperatur for the parameter of the first term of the
Henyey-Greenstein atmospheric phase function.
This parameter gives the range over which random guesses can be expected to
vary at first:
HG1_ATM_NEW = T_HG1_ATM * tan( PI * ran_num + PI/2 ).
As the system cools the range will constrict gradually :
T_HG1_ATM_NEW_* = T_HG1_ATM_OLD_* * scale,
scale depends of NUMTEN.