A medium type in the atmosphere that only absorbs light with two layers. In Earth's atmosphere this is used to model ozone.
Computed as:
extinction * (linearTerm * h + constantTerm), Copy
extinction * (linearTerm * h + constantTerm),
where h is the altitude and linearTerm and constantTerm are the first or second layer's linear and constant terms. If h is lower than AbsorptionLayer0.height, Absorption.layer0 is used, otherwise Absorption.layer1 is used.
h
linearTerm
constantTerm
The extinction coefficients of the absorption component in km^-1.
km^-1
The lower layer of the absorption component.
The upper layer of the absorption component.
A medium type in the atmosphere that only absorbs light with two layers. In Earth's atmosphere this is used to model ozone.
Computed as:
where
h
is the altitude andlinearTerm
andconstantTerm
are the first or second layer's linear and constant terms. Ifh
is lower than AbsorptionLayer0.height, Absorption.layer0 is used, otherwise Absorption.layer1 is used.