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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Ground-based validation of EOS-Aura OMI NO2 vertical column data in the midlatitude mountain ranges of Tien Shan (Kyrgyzstan) and Alps (France)
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Ground-based validation of EOS-Aura OMI NO2 vertical column data in the midlatitude mountain ranges of Tien Shan (Kyrgyzstan) and Alps (France)

机译:地面EOS-Aura OMI NO2的验证在山中间纬度垂直列数据天山山脉(吉尔吉斯斯坦)和阿尔卑斯山(法国)

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摘要

Ground-based UV-visible instruments for NO2 vertical column measurements have been operating at Issyk-Kul station, in Kyrgyzstan, and Observatoire de Haute-Provence (OHP), in France, since 1983 and 1992, respectively. These measurements have already been used for validation of ERS-2 Global Ozone Monitoring Experiment (GOME) and Envisat Scanning Imaging Absorption Spectrometer for Atmospheric Cartography (SCIAMACHY) NO2 column data. Building upon the successful missions of GOME and SCIAMACHY, the Ozone Monitoring Experiment (OMI) was launched by NASA onboard the EOS Aura satellite in July 2004. Here we present the results of recent comparisons between OMI NO2 operational data (standard product) and correlative ground-based twilight measurements in midlatitudes, at Issyk-Kul and OHP, in 2004–2006. The stratospheric NO2 columns, observed by OMI and our ground-based instruments, have been corrected for NO2 diurnal change and normalized to local noon values using a photochemical box model. According to our comparison, OMI stratospheric NO2 columns underestimate ground-based measurements by (0.3 ± 0.3) × 1015 molecules/cm2 and (0.7 ± 0.6) × 1015 molecules/cm2 at Issyk-Kul and OHP, respectively. The effect of tropospheric pollution on the NO2 measurements in both regions of observations has been identified and discussed.
机译:地面紫外可见NO2的仪器垂直列测量操作在吉尔吉斯斯坦,在吉站自1983年和1992年,分别。已经被用于测量验证ERS-2全球臭氧监测(国美)和环境扫描成像实验吸收光谱仪大气制图(模拟战)NO2列数据。国美的成功的任务模拟战,臭氧监测实验(OMI)由NASA发射机上EOS光环卫星在2004年7月。最近比较OMI NO2的结果(标准产品)和操作数据相关地面《暮光之城》的测量情理之中,在吉和形成,在2004 - 2006。平流层NO2列,观察到尾身茂和我们的地面仪器,纠正对NO2昼夜变化和规范化当地中午值使用光化学盒子模型。平流层NO2列低估地面测量的(0.3±0.3)×1015分子/ cm2和(0.7±0.6)×1015分别在吉分子/ cm2,形成。的影响对流层NO2污染这两个地区的测量的观测被确认和讨论。

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