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Tropospheric ozone and ozone profiles retrieved from GOME-2 and their validation

机译:从GOME-2提取的对流层臭氧和臭氧剖面及其验证

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This paper describes and assesses the performance of the RAL (Rutherford Appleton Laboratory) ozone profile retrieval scheme for the Global Ozone Monitoring Experiment 2 (GOME-2) with a focus on tropospheric ozone. Developments to the scheme since its application to GOME-1 measurements are outlined. These include the approaches developed to account sufficiently for UV radiometric degradation in the Hartley band and for inadequacies in knowledge of instrumental parameters in the Huggins bands to achieve the high-precision spectral fit required to extract information on tropospheric ozone. brbr The assessment includes a validation against ozonesondes (sondes) sampled worldwide over 2 years (2007–2008). Standard deviations of the ensemble with respect to the sondes are considerably lower for the retrieved profiles than for the a priori, with the exception of the lowest subcolumn. Once retrieval vertical smoothing (averaging kernels) has been applied to the sonde profiles there is a retrieval bias of 6% (1.5 DU) in the lower troposphere, with smaller biases in the subcolumns above. The bias in the troposphere varies with latitude. The retrieval underestimates lower tropospheric ozone in the Southern Hemisphere (SH) (15–20% or ~ 1–3 DU) and overestimates it in the Northern Hemisphere (NH) (10% or 2 DU). brbr The ability of the retrieval to reflect the geographical distribution of lower tropospheric ozone, globally (rather than just ozonesonde launch sites) is demonstrated by comparison with the chemistry transport model TOMCAT. For a monthly mean of cloud-cleared GOME-2 pixels, a correlation of 0.66 is found between the retrieval and TOMCAT sampled accordingly, with a bias of 0.7 Dobson Units. GOME-2 estimates higher concentrations in NH pollution centres but lower ozone in the Southern Ocean and South Pacific, which is consistent with the comparison to ozonesondes.
机译:本文介绍并评估了针对全球对流层臭氧的全球臭氧监测实验2(GOME-2)的RAL(卢瑟福·阿普尔顿实验室)臭氧分布图检索方案的性能。概述了该方案自应用于GOME-1测量以来的发展。这些方法包括开发的方法,这些方法足以解决Hartley波段中的UV辐射衰减问题以及Huggins波段中仪器参数知识的不足,无法获得提取对流层臭氧信息所需的高精度光谱拟合。 评估包括对过去2年(2007-2008年)在全球范围内采样的臭氧探空仪(探空仪)的验证。除最低的子列外,对于检索到的轮廓,集合相对于主机的标准偏差要比先验的低得多。一旦将取回垂直平滑(平均内核)应用于探空仪剖面,在对流层下部,取回偏差为6%(1.5 DU),上方子列的取回偏差较小。对流层的偏差随纬度变化。反演结果低估了南半球(SH)的对流层较低的臭氧(15–20%或〜1-3 DU),而高估了北半球(NH)的对流层臭氧(10%或2 DU)。 通过与化学传输模型TOMCAT进行比较,证明了该检索具有反映全球低层对流层臭氧的地理分布的能力(而不仅仅是臭氧探空仪的发射场)。对于清除云的GOME-2像素的月平均值,在取回和相应采样的TOMCAT之间发现0.66的相关性,偏差为0.7 Dobson单位。 GOME-2估计,NH污染中心的浓度较高,而南大洋和南太平洋的臭氧含量较低,这与臭氧探空仪的比较是一致的。

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