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首页> 外文期刊>Atmospheric Chemistry and Physics Discussions >Global CFC-11 (CClsub3/subF) and CFC-12 (CClsub2/subFsub2/sub) measurements with the Michelson Interferometer for Passive Atmospheric Sounding (MIPAS): retrieval, climatologies and trends
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Global CFC-11 (CClsub3/subF) and CFC-12 (CClsub2/subFsub2/sub) measurements with the Michelson Interferometer for Passive Atmospheric Sounding (MIPAS): retrieval, climatologies and trends

机译:迈克尔逊干涉仪用于被动大气探测的全球CFC-11(CCl 3 F)和CFC-12(CCl 2 F 2 )测量( MIPAS):检索,气候和趋势

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pstrongAbstract./strong Vertical profiles of CFC-11 (CClsub3/subF) and CFC-12 (CClsub2/subFsub2/sub) have been measured with the Michelson Interferometer for Passive Atmospheric Sounding (MIPAS) with global coverage under daytime and nighttime conditions. The profile retrieval is based on constrained nonlinear least squares fitting of measured limb spectral radiance to modeled spectra. CFC-11 is measured in its νsub4/sub-band at 850 cmsupa??1/sup, and CFC-12 is analyzed in its νsub6/sub-band at 922 cmsupa??1/sup. To stabilize the retrievals, a Tikhonov-type smoothing constraint is applied. Main retrieval error sources are measurement noise and elevation pointing uncertainties. The estimated CFC-11 retrieval errors including noise and parameter errors but excluding spectroscopic data uncertainties are below 10 pptv in the middle stratosphere, depending on altitude, the MIPAS measurement mode and the actual atmospheric situation. For CFC-12 the total retrieval errors are below 28 pptv at an altitude resolution varying from 3 to 5 km. Time series of altitude/latitude bins were fitted by a simple parametric approach including constant and linear terms, a quasi-biennial oscillation (QBO) proxy and sine and cosine terms of several periods. In the time series from 2002 to 2011, quasi-biennial and annual oscillations are clearly visible. A decrease of stratospheric CFC mixing ratios in response to the Montreal Protocol is observed for most altitudes and latitudes. However, the trends differ from the trends measured in the troposphere, they are even positive at some latitudes and altitudes, and can in some cases only be explained by decadal changes in atmospheric age of air spectra or vertical mixing patterns./p.
机译:> >摘要。CFC-11(CCl 3 F)和CFC-12(CCl 2 F 2 < / sub>)已通过迈克尔逊被动大气探测干涉仪(MIPAS)进行了测量,其白天和黑夜条件下的全球覆盖范围都得到了改善。轮廓检索基于所测肢体光谱辐射度对建模光谱的约束非线性最小二乘法拟合。在850 cm a ?? 1 的&n; 4 波段中测量CFC-11,并在&nu; 6 中分析CFC-12。 922 cm a ?? 1 的sub> -band。为了稳定检索,应用了Tikhonov型平滑约束。主要的检索误差源是测量噪声和高程指向不确定性。在平流层中层,估计的CFC-11检索误差(包括噪声和参数误差,但不包括光谱数据不确定性)低于10 pptv,具体取决于海拔高度,MIPAS测量模式和实际大气情况。对于CFC-12,在3至5 km的海拔分辨率下,总的检索误差低于28 pptv。高度/纬度区间的时间序列通过简单的参数方法进行拟合,包括常数项和线性项,准两年一次振荡(QBO)代理以及多个周期的正弦和余弦项。在2002年至2011年的时间序列中,准双年度和年度振荡清晰可见。在大多数海拔和纬度上,观察到响应《蒙特利尔议定书》的平流层CFC混合比降低。但是,这种趋势不同于对流层中测得的趋势,在某些纬度和高度甚至是正的,并且在某些情况下只能用大气年龄的年代际变化或垂直混合模式来解释。

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