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Rotational Raman scattering in the Earth's atmosphere ... - SRON

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32 Chapter 2<br />

<strong>scatter<strong>in</strong>g</strong> event. In both cases <strong>the</strong> nth order term of <strong>the</strong> Dyson series represents <strong>the</strong> contribution of<br />

n order of <strong>Raman</strong> <strong>scatter<strong>in</strong>g</strong> to <strong>the</strong> Green’s operator G. For numerical applications, we truncate <strong>the</strong><br />

Dyson series <strong>in</strong> first order, hence<br />

G ≈ G o − G o ∆LG o . (2.23)<br />

Now <strong>the</strong> differences between <strong>the</strong> two applications of <strong>the</strong> perturbation <strong>the</strong>ory become clear, i.e. result<strong>in</strong>g<br />

from <strong>the</strong> <strong>the</strong> different choice of both G 0 and ∆L. In <strong>the</strong> case of <strong>the</strong> unperturbed problem<br />

<strong>in</strong>clud<strong>in</strong>g purely Cabannes <strong>scatter<strong>in</strong>g</strong>, <strong>Raman</strong> <strong>scatter<strong>in</strong>g</strong> processes of second order and higher are ignored,<br />

whereas <strong>in</strong> <strong>the</strong> second case <strong>the</strong>se <strong>scatter<strong>in</strong>g</strong> processes are effectively described by Rayleigh<br />

<strong>scatter<strong>in</strong>g</strong>. In that sense both applications correspond to approaches A and B mentioned above. The<br />

correspond<strong>in</strong>g numerical applications of <strong>the</strong> perturbation <strong>the</strong>ory will be referred to as <strong>the</strong> PTA and <strong>the</strong><br />

PTB model.<br />

First of all, we compared PTA model simulations with DA1 simulations. Here it is important<br />

to notice that, although both models describe multiple Cabannes <strong>scatter<strong>in</strong>g</strong> and one order of <strong>Raman</strong><br />

<strong>scatter<strong>in</strong>g</strong>, <strong>the</strong>y do not solve exactly <strong>the</strong> same problem. The DA1 model takes <strong>in</strong>to account that a<br />

<strong>Raman</strong> <strong>scatter<strong>in</strong>g</strong> event <strong>in</strong>fluences <strong>the</strong> succeed<strong>in</strong>g propagation of light. This is not <strong>the</strong> case for <strong>the</strong><br />

PTA model. The propagation before and after <strong>the</strong> perturbation is kept fixed, as can be seen <strong>in</strong> <strong>the</strong><br />

second term <strong>in</strong> Eq. (2.23), where G o describes <strong>the</strong> propagation of scattered light <strong>in</strong> a pure Cabannes<br />

<strong>scatter<strong>in</strong>g</strong> <strong>atmosphere</strong>. However, <strong>the</strong> model simulations show that this is only a m<strong>in</strong>or effect that<br />

causes differences less than 0.005% between <strong>the</strong> simulated radiance spectra.<br />

Figure 2.5: Absolute difference <strong>in</strong> fill<strong>in</strong>g-<strong>in</strong> between <strong>the</strong> perturbation <strong>the</strong>ory model result (PTA and PTB)<br />

and <strong>the</strong> doubl<strong>in</strong>g-add<strong>in</strong>g model result (DA). L<strong>in</strong>es are drawn for approach A (PTA, dotted l<strong>in</strong>e), where a<br />

Cabannes <strong>scatter<strong>in</strong>g</strong> <strong>atmosphere</strong> is taken as <strong>the</strong> base problem, and for approach B (PTB, solid l<strong>in</strong>e), where<br />

a Rayleigh <strong>scatter<strong>in</strong>g</strong> <strong>atmosphere</strong> is taken as <strong>the</strong> base problem. The same model parameters were used as<br />

<strong>in</strong> Fig. 2.4.<br />

Fig. 2.5 presents <strong>the</strong> comparison of both PTA and PTB model simulations with DA simulations,<br />

which <strong>in</strong>clude multiple <strong>Raman</strong> <strong>scatter<strong>in</strong>g</strong>. Shown is <strong>the</strong> absolute difference <strong>in</strong> <strong>the</strong> fill<strong>in</strong>g-<strong>in</strong> spectra

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