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Vegetation Radiative Transfer Modelling (Nadine Gobron) - PEER

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Optical thickness<br />

• The variable physical depth can be multiplied by the<br />

optical factor S+K=E to transform into an optical thickness<br />

↓<br />

∂I<br />

(z)<br />

∂τ<br />

τ<br />

= −I<br />

↓<br />

z<br />

∂z<br />

= ∫ (S + K) ∂z<br />

0<br />

(1 + g)<br />

(z) + ω<br />

2<br />

I<br />

↓<br />

(1 − g)<br />

(z) + ω<br />

2<br />

I<br />

↑<br />

(z)<br />

∂τ<br />

(1)<br />

↑<br />

∂I<br />

(z)<br />

∂τ<br />

= + I<br />

↑<br />

(z)<br />

−<br />

ω<br />

(1 + g)<br />

2<br />

I<br />

↑<br />

(z)<br />

−<br />

ω<br />

(1 − g)<br />

2<br />

I<br />

↓<br />

(z)<br />

(2)<br />

These last equations are typical two-stream equations<br />

for the system.<br />

Pinty, B. and M. M. Verstraete (1998) `Introduction to Radiation <strong>Transfer</strong> Modeling in Geophysical Media’, in From Urban<br />

Air Pollution to Extra-Solar Planets, ERCA Volume 3 Edited by C. Boutron, EDP Sciences, Les Ulis, France, 67-87.<br />

18

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