If an option other than NONE is selected, an atmospheric scattering
and surface photometric properties are included as
part of the physical model to which the empirical model is fitted.
Six available atmospheric models are categorized into three
classes that differ in their treatment of the single particle
scattering function for atmospheric particles. Each of these classes
of model can be evaluated to a first order (faster) or second order
(more accurate) approximation. Atmospheric scattering in all these
models both attenuates the surface signal and adds its own (uniform)
contribution to the image
radiance.
Therefore, unless NONE is selected, it makes sense to also set
ADDOFFSET=YES so that the additive contribution of the atmosphere
will be modeled by an additive constant in the fit. This approach
is useful in preparing for photoclinometry (shape from shading),
for which images are normally preprocessed by subtracting a uniform
haze component that corresponds to the additive term in the fit with
ADDOFFSET=YES.
Type
| combo |
Default
|
NONE
|
Internal Default
| NONE |
Option List:
|
Option |
Brief |
Description |
NONE |
No atmospheric scattering model
|
The radiance from the Hapke surface
is not modified by atmospheric scattering.
Exclusions
- TAU
- WHA
- HGA
- HNORM
- ADDOFFSET
- BHA
|
ISOTROPIC1 |
First order isotropic
|
Atmospheric particles are assumed to scatter light isotropically.
The effects of this scattering are calculated exactly to first
order.
Exclusions
Inclusions
|
ISOTROPIC2 |
Second order isotropic
|
Atmospheric particles are assumed to scatter light isotropically.
The effects of this scattering are calculated exactly to second
order.
Exclusions
Inclusions
|
ANISOTROPIC1 |
First order anisotropic
|
Atmospheric particles are assumed to scatter light according
to a Legendre polynomial model with a single term. The effects
of this scattering are calculated exactly to first order.
Exclusions
Inclusions
- TAU
- WHA
- BHA
- HNORM
- ADDOFFSET
|
ANISOTROPIC2 |
Second order anisotropic
|
Atmospheric particles are assumed to scatter light according to
a Legendre polynomial model with a single term. The effects of
this scattering are calculated exactly to second order.
Exclusions
Inclusions
- TAU
- WHA
- BHA
- HNORM
- ADDOFFSET
|
HAPKEATM1 |
First order Henyey-Greenstein
|
Atmospheric particles are assumed to scatter light according to
a single parameter Henyey-Greenstein function (see the description
of the surface scattering parameter HG1 for the equation that
combines two such functions for surface particles). The effects
of this scattering are approximated by using a first order solution
for multiple scattering by isotropic particles and making a
correction to the distribution of singly scattered radiation. The
model is called HAPKEATM1 because this correction for the single
particle phase function is similar to the one developed by Hapke
(1981) for surface scattering.
Exclusions
Inclusions
- TAU
- WHA
- HGA
- HNORM
- ADDOFFSET
|
HAPKEATM2 |
Second order Henyey-Greenstein
|
Atmospheric particles are assumed to scatter light according to
a single parameter Henyey-Greenstein function (see the description
of the surface scattering parameter HG1 for the equation that
combines two such functions for surface particles). The effects
of this scattering are approximated by using a second order solution
for multiple scattering by isotropic particles and making a
correction to the distribution of singly scattered radiation. The
model is called HAPKEATM2 because this correction for the single
particle phase function is similar to the one developed by Hapke
(1981) for surface scattering.
Exclusions
Inclusions
- TAU
- WHA
- HGA
- HNORM
- ADDOFFSET
|
|
This is the normal atmospheric optical depth.
Type
| double |
Internal Default
| None Specified |
Minimum
| 0.0
(inclusive)
|
This is the single-scattering
albedo of atmospheric
particles, not to be confused with the albedo WH of surface particles.
Type
| double |
Internal Default
| None Specified |
Minimum
| 0.0
(exclusive)
|
Maximum
| 1.0
(inclusive)
|
Parameter used in the Henyey-Greenstein single particle phase
function for atmospheric particles when ATMNAME=HAPKEATM1 or
ATMNAME=HAPKEATM2. This is the asymmetry parameter for a single
term Henyey-Greenstein model:
p(phase) = (1-hga**2)/(1+hga**2+2*hga*cos(phase))**1.5
Not to be confused with corresponding parameter HG1 for the
surface particles.
Type
| double |
Internal Default
| None Specified |
Minimum
| -1.0
(exclusive)
|
Maximum
| 1.0
(exclusive)
|
Coefficient of the first order Legendre polynomial in the
single particle phase function for atmospheric scattering.
When ATMNAME=ANISOTROPIC1 or ATMNAME=ANISOTROPIC2, a two-term
Legendre polynomial expansion is used to represent the
scattering phase function of single particles in the atmosphere:
p(phase) = 1 + bha * p1(cos(phase))
Where, P1 is the first order Legendre polynomial, and not to be
confused with the corresponding parameter BH for the surface.
Type
| double |
Internal Default
| None Specified |
Minimum
| -1.0
(inclusive)
|
Maximum
| 1.0
(inclusive)
|
Atmospheric shell thickness normalized to planet radius, used
to correct the path lengths of atmospheric transmission for the
spherical geometry of the planet. Default 0.003 is for Mars.
Type
| double |
Internal Default
| None Specified |
Minimum
| 0.0
(inclusive)
|
If true, the additive contribution of the atmosphere will be modeled
by an additive constant in the fit of the empirical function at each
phase angle.
Type
| boolean |
Default
|
false
|