Single-scattering albedo of the soil particles; 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.
Parameter which characterizes the soil structure (angular width of the 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.
Parameter of the first term of the Legendre-Polynomial soil particle phase function.
This parameter gives the absolut lower limit of the parameter of the first term of the Legendre-Polynomial 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 Legendre-Polynomial 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
Legendre-Polynomial soil particle phase function.
This parameter gives the range over which random guesses can be expected to
vary at first:
LE1_SOIL_NEW = T_LE1_SOIL * tan( PI * ran_num + PI/2 ).
As the system cools the range will constrict gradually :
T_LE1_SOIL_NEW_* = T_LE1_SOILE_OLD_* * scale,
scale depends of NUMTEN.
Parameter of the second term of the Legendre-Polynomial soil particle phase function.
This parameter gives the absolut lower limit of the parameter of the second term of the Legendre-Polynomial 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 second term of the Legendre-Polynomial 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 second term of the
Legendre-Polynomial soil particle phase function.
This parameter gives the range over which random guesses can be expected to
vary at first:
LE2_SOIL_NEW = T_LE2_SOIL * tan( PI * ran_num + PI/2 ).
As the system cools the range will constrict gradually :
T_LE2_SOIL_NEW_* = T_LE2_SOIL_OLD_* * scale,
scale depends of NUMTEN.