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Improving atmospheric CO\u3csub\u3e2\u3c/sub\u3e retrievals using line mixing and speed-dependence when fitting high-resolution ground-based solar spectra

机译:当拟合高分辨率的地面太阳光谱时,使用线混合和速度相关性来改善大气CO \ u3csub \ u3e2 \ u3c / sub \ u3e检索

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摘要

A quadratic speed-dependent Voigt spectral line shape with line mixing (qSDV + LM) has been included in atmospheric trace-gas retrievals to improve the accuracy of the calculated CO2 absorption coefficients. CO2 laboratory spectra were used to validate absorption coefficient calculations for three bands: the strong 20013 ← 00001 band centered at 4850 cm−1, and the weak 30013 ← 00001 and 30012 ← 00001 bands centered at 6220 cm−1 and 6340 cm−1 respectively, and referred to below as bands 1 and 2. Several different line lists were tested. Laboratory spectra were best reproduced for the strong CO2 band when using HITRAN 2008 spectroscopic data with air-broadened widths divided by 0.985, self-broadened widths divided by 0.978, line mixing coefficients calculated using the exponential power gap (EPG) law, and a speed-dependent parameter of 0.11 used for all lines. For the weak CO2 bands, laboratory spectra were best reproduced using spectroscopic parameters from the studies by Devi et al. in 2007 coupled with line mixing coefficients calculated using the EPG law. A total of 132,598 high-resolution ground-based solar absorption spectra were fitted using qSDV + LM to calculate CO2 absorption coefficients and compared to fits that used the Voigt line shape. For the strong CO2 band, the average root mean square (RMS) residual is 0.49 ± 0.22% when using qSDV + LM to calculate the absorption coefficients. This is an improvement over the results with the Voigt line shape, which had an average RMS residual of 0.60 ± 0.21%. When using the qSDV + LM to fit the two weak CO2 bands, the average RMS residual is 0.47 ± 0.19% and 0.51 ± 0.20% for bands 1 and 2, respectively. These values are identical to those obtained with the Voigt line shape. Finally, we find that using the qSDV + LM decreases the airmass dependence of the column averaged dry air mole fraction of CO2 retrieved from the strong and both weak CO2 bands when compared to the retrievals obtained using the Voigt line shape.
机译:大气中痕量气体的回采中已包含二次线性混合的速度依赖性Voigt谱线形状(qSDV + LM),以提高计算出的CO2吸收系数的准确性。使用CO2实验室光谱来验证三个波段的吸收系数计算:分别以4850 cm-1为中心的强20013←00001带和分别以6220 cm-1和6340 cm-1为中心的30013←00001和30012←00001弱带,以下称为频段1和2。测试了几种不同的线路列表。当使用HITRAN 2008光谱数据进行空气扩展宽度除以0.985,自扩展宽度除以0.978,使用指数幂差距(EPG)律计算的线混合系数时,实验室光谱在强CO2波段上的再现效果最佳。用于所有行的与参数相关的参数0.11。对于较弱的CO2波段,最好使用Devi等人研究的光谱参数来重现实验室光谱。 2007年,再加上使用EPG法则计算的线路混合系数。使用qSDV + LM拟合了总共132,598个高分辨率的地面日光吸收光谱,以计算CO2吸收系数,并与使用Voigt线形的拟合进行了比较。对于强CO2带,当使用qSDV + LM计算吸收系数时,平均均方根(RMS)残留为0.49±0.22%。这是对Voigt线形结果的改进,该形状的平均RMS残差为0.60±0.21%。当使用qSDV + LM拟合两个弱CO2频带时,频带1和2的平均RMS残留分别为0.47±0.19%和0.51±0.20%。这些值与使用Voigt线形获得的值相同。最后,我们发现,与使用Voigt线形获得的回采相比,使用qSDV + LM可以降低从强和弱两个CO2带中检索到的平均CO2柱平均干燥空气摩尔分数的气质依赖性。

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