Rotational Raman scattering in the Earth's atmosphere ... - SRON
Rotational Raman scattering in the Earth's atmosphere ... - SRON
Rotational Raman scattering in the Earth's atmosphere ... - SRON
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72 Chapter 3<br />
where λ is <strong>the</strong> wavelength of <strong>the</strong> <strong>in</strong>com<strong>in</strong>g light and λ ′ represents <strong>the</strong> correspond<strong>in</strong>g wavelength of<br />
<strong>the</strong> scattered light. f(T,J) is <strong>the</strong> fractional population <strong>in</strong> <strong>the</strong> <strong>in</strong>itial state and can be approximated by<br />
[Jo<strong>in</strong>er et al., 1995]<br />
f(T,J) = 1 [<br />
g(J) [2J+1] exp<br />
N f<br />
− E(J)<br />
kT<br />
]<br />
, (3.74)<br />
where g is <strong>the</strong> nuclear sp<strong>in</strong> statistical weight factor, k is <strong>the</strong> Boltzmann’s constant, T is <strong>the</strong> temperature,<br />
and E(J) = hcBJ(J +1) is <strong>the</strong> rotational energy (h is Planck’s constant, c is <strong>the</strong> speed of<br />
light, and B is <strong>the</strong> rotational constant). The coefficient N f can be determ<strong>in</strong>ed from <strong>the</strong> normalization<br />
condition<br />
∑<br />
f(T,J) = 1. (3.75)<br />
J<br />
b(J → J ′ ) represents <strong>the</strong> Placzek-Teller coefficient for <strong>the</strong> transition J → J ′ . For simple l<strong>in</strong>ear<br />
molecules <strong>the</strong>se coefficients are given by<br />
b(J →J+2) = 3(J+1)(J+2)<br />
2(2J+1)(2J+3) , (3.76)<br />
for Stokes l<strong>in</strong>es and<br />
b(J →J −2) =<br />
3J(J −1)<br />
2(2J −1)(2J+3) , (3.77)<br />
for anti-Stokes l<strong>in</strong>es. The change <strong>in</strong> wavelength ∆λ=λ ′ −λ due to rotational <strong>Raman</strong> <strong>scatter<strong>in</strong>g</strong> can be<br />
calculated easily from <strong>the</strong> energy difference between <strong>the</strong> <strong>in</strong>itial and f<strong>in</strong>al state, ∆E = E(J ′ )−E(J).<br />
The <strong>scatter<strong>in</strong>g</strong> phase matrix P, def<strong>in</strong>ed with respect to <strong>the</strong> plane of <strong>scatter<strong>in</strong>g</strong>, has <strong>the</strong> same structure<br />
Table 3.1: Parameters A, B, C, and normalization constant N of <strong>scatter<strong>in</strong>g</strong> phase function (3.78) for<br />
Rayleigh, Cabannes and rotational <strong>Raman</strong> <strong>scatter<strong>in</strong>g</strong>.<br />
A B C N<br />
Rayleigh 3(45+ε) 30(9−ε) 36ε (180+40ε)<br />
Cabannes 3(180+ε) 30(36−ε) 36ε 40(18+ε)<br />
rot. <strong>Raman</strong> 3 −30 36 40<br />
for Rayleigh, Cabannes and rotational <strong>Raman</strong> <strong>scatter<strong>in</strong>g</strong>, viz.<br />
⎛<br />
⎞<br />
A(1+cos 2 Θ) + C −A(1−cos 2 Θ) 0 0<br />
P(Θ) =<br />
1 −A(1−cos 2 Θ) A(1+cos 2 Θ) 0 0<br />
⎜<br />
⎟<br />
N ⎝ 0 0 2A cos Θ 0 ⎠<br />
0 0 0 B cos Θ<br />
(3.78)