TY - JOUR
T1 - Non-Voigt line-shape effects on retrievals of atmospheric ozone
T2 - Line-mixing effects
AU - Tran, H.
AU - Picquet-Varrault, B.
AU - Boursier, C.
AU - Viatte, C.
AU - Eremenko, M.
AU - Hase, F.
AU - Hartmann, J. M.
PY - 2011/9/1
Y1 - 2011/9/1
N2 - A theoretical approach is proposed to model line-mixing (LM) effects on absorption coefficients of O3 perturbed by N2 and air. It uses state-to-state rotational cross-sections calculated with a semi-classical approach and two empirical parameters, which enable switching from the state space to the line space. The first, associated with couplings within Q branches is deduced from a room temperature far-infrared spectrum. The second, governing line-couplings between R (or P) lines, is determined from a spectrum measured in the v1+v2+v3 band. The model developed is then successfully compared with measurements performed at room temperature for a relatively large range of pressure (0.7-8atm) and in four different bands (from 3 to 300μm). Accurate predictions are, in particular, obtained in the 10γm (v1, v3) region, which is widely used for remote sensing purposes. Consequences of LM effects on retrievals of ozone atmospheric volume mixing ratios are then studied using simulated atmospheric spectra. The results show that LM leads to systematic spectra fit residuals and errors on the retrieved ozone amounts, which are small but might be detectable in measured atmospheric spectra.
AB - A theoretical approach is proposed to model line-mixing (LM) effects on absorption coefficients of O3 perturbed by N2 and air. It uses state-to-state rotational cross-sections calculated with a semi-classical approach and two empirical parameters, which enable switching from the state space to the line space. The first, associated with couplings within Q branches is deduced from a room temperature far-infrared spectrum. The second, governing line-couplings between R (or P) lines, is determined from a spectrum measured in the v1+v2+v3 band. The model developed is then successfully compared with measurements performed at room temperature for a relatively large range of pressure (0.7-8atm) and in four different bands (from 3 to 300μm). Accurate predictions are, in particular, obtained in the 10γm (v1, v3) region, which is widely used for remote sensing purposes. Consequences of LM effects on retrievals of ozone atmospheric volume mixing ratios are then studied using simulated atmospheric spectra. The results show that LM leads to systematic spectra fit residuals and errors on the retrieved ozone amounts, which are small but might be detectable in measured atmospheric spectra.
KW - Atmospheric spectra
KW - Line-mixing
KW - Line-shape
KW - Ozone
KW - Spectroscopic parameters
U2 - 10.1016/j.jqsrt.2011.06.001
DO - 10.1016/j.jqsrt.2011.06.001
M3 - Article
AN - SCOPUS:80051569263
SN - 0022-4073
VL - 112
SP - 2287
EP - 2295
JO - Journal of Quantitative Spectroscopy and Radiative Transfer
JF - Journal of Quantitative Spectroscopy and Radiative Transfer
IS - 14
ER -