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首页> 外文期刊>Atmospheric chemistry and physics >Retrieval of nitrogen dioxide stratospheric profiles from ground-based zenith-sky UV-visible observations: validation of the technique through correlative comparisons
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Retrieval of nitrogen dioxide stratospheric profiles from ground-based zenith-sky UV-visible observations: validation of the technique through correlative comparisons

机译:从地面天顶天顶紫外可见观测值中检索二氧化氮平流层剖面:通过相关比较对该技术进行验证

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A retrieval algorithm based on the Optimal Estimation Method (OEM) has beendeveloped in order to provide vertical distributions of NO2 in thestratosphere from ground-based (GB) zenith-sky UV-visible observations. Ithas been applied to observational data sets from the NDSC (Network forDetection of Stratospheric Change) stations of Harestua (60° N, 10° E)and Andøya (69° N, 16° E) in Norway. The information contentand retrieval errors have been analyzed following a formalism used forcharacterizing ozone profiles retrieved from solar infrared absorptionspectra. In order to validate the technique, the retrieved NO2 verticalprofiles and columns have been compared to correlative balloon and satelliteobservations. Such extensive validation of the profile and column retrievalswas not reported in previously published work on the profiling from GBUV-visible measurements. A good agreement - generally better than 25% - has beenfound with the SAOZ (Système d'Analyse par ObservationsZénithales) and DOAS (Differential Optical Absorption Spectroscopy)balloons. A similar agreement has been reached with correlativesatellite data from the HALogen Occultation Experiment (HALOE) and Polar Ozoneand Aerosol Measurement (POAM) III instruments above 25km of altitude.Below 25km, a systematic underestimation - by up to 40% in some cases - of bothHALOE and POAM III profiles by our GB profile retrievals has been observed,pointing out more likely a limitation of both satellite instruments at these altitudes.We have concluded that our study strengthens our confidence in the reliability of theretrieval of vertical distribution information from GB UV-visible observations andoffers new perspectives in the use of GB UV-visible network data for validation purposes.
机译:为了提供平地层NO 2 在地面(GB)天顶天空紫外可见观测值的垂直分布,开发了一种基于最优估计方法(OEM)的检索算法。它已被应用于挪威Harestua(60°N,10°E)和Andøya(69°N,16°E)的NDSC(平流层变化检测网络)站的观测数据集。按照用于表征从太阳红外吸收光谱中检索到的臭氧剖面的形式化方法,分析了信息内容和检索错误。为了验证该技术,已将检索到的NO 2 垂直剖面和列与相关的气球和卫星观测进行了比较。在以前发表的关于从GBUV可见的测量结果进行分析的工作中,没有报告过这种对轮廓和列检索的广泛验证。已经与SAOZ(Systèmed'Analyse parobservationsZénithales)和DOAS(差分光吸收光谱)气球达成了良好的协议-通常优于25%。在海拔25公里以上的HALogen掩星实验(HALOE)和极地臭氧和气溶胶测量(POAM)III仪器中获得的相关卫星数据也达成了类似的协议。在25km以下,这两个系统都被系统低估了-在某些情况下最高可达40%通过GB廓线检索得到的POAM III和POAM III廓线,更可能指出了这两个卫星在这些高度上的局限性。我们的结论是,我们的研究增强了我们对从GB紫外线可见的垂直分布信息的可靠性的信心。观察并提供了使用GB紫外线可见网络数据进行验证的新观点。

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