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Ground-based FTIR measurements at Ile de La Réunion: Observations, error analysis and comparisons with satellite data.

机译:留尼汪岛的地面FTIR测量:观测,误差分析以及与卫星数据的比较。

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摘要

Ground-based Fourier-transform infrared (FTIR) spectroscopy is a powerful remote sensing technique to obtain information on the total column abundances and on the vertical distribution of various constituents in the atmosphere. Many of these species are essential for the investigation of important atmospheric phenomena, such as the overall greenhouse effect or the stratospheric ozone decrease and recovery.In the frame of the Network for the Detection of Atmospheric Composition Change (NDACC), such observations have been made since many years at several measurement stations for the worldwide long-term monitoring of the atmospheric composition. In this work, we present the results from two short-term FTIR measurement campaigns in 2002 and 2004 at the Ile de La Réunion (21°S, 55°E), a complementary NDACC site in the subtropics, in the Indian Ocean. All spectra were recorded in solar absorption mode.The results discussed here concern the direct greenhouse gases methane (CH4), nitrous oxide (N2O) and ozone (O3), and the indirect greenhouse gases carbon monoxide (CO) and ethane (C2H6), as well as hydrogen cyanide (HCN) and stratospheric hydrogen chloride (HCl), hydrogen fluoride (HF) and nitric acid (HNO3). For the latter species (HCN, HCl, HF and HNO3), we show time series of total column amounts from the surface up to 60 km. For CO, CH4, N2O and O3, it is possible to derive additionally independent information on a few partial columns; these time series are discussed as well. A complete error budget of the retrieval products is given.Temporary mutually correlated enhancements of CO, C2H6and HCN have been observed.They have been traced back to biomass burning events in southern Africa and Madagascar using the FLEXPART model.Comparisons of our retrievals with correlative data from satellite experiments, such as ACE and MOPITT, and with available ozone soundings, show generally good agreements between the different data sets.
机译:地面傅立叶变换红外(FTIR)光谱技术是一种强大的遥感技术,可获取有关总色谱柱丰度和大气中各种成分的垂直分布的信息。这些物种中的许多对于调查重要的大气现象(例如整体温室效应或平流层臭氧的减少和恢复)是必不可少的。在大气成分变化检测网络(NDACC)的框架中,已经进行了此类观察多年来在多个测量站进行了全球范围的大气成分长期监测。在这项工作中,我们介绍了2002年和2004年在印度洋副热带地区NDACC互补地点Ile de LaRéunion(21°S,55°E)的两个短期FTIR测量活动的结果。所有光谱均以太阳吸收模式记录,此处讨论的结果涉及直接温室气体甲烷(CH4),一氧化二氮(N2O)和臭氧(O3)以及间接温室气体一氧化碳(CO)和乙烷(C2H6),以及氰化氢(HCN)和平流层氯化氢(HCl),氟化氢(HF)和硝酸(HNO3)。对于后一种(HCN,HCl,HF和HNO3),我们显示了从地表直至60 km的总柱量的时间序列。对于CO,CH4,N2O和O3,可以在几个部分列上另外获得独立的信息;例如,还讨论了这些时间序列。给出了回收产品的完整误差预算,观察到了CO,C2H6和HCN的暂时相互关联的增强,并使用FLEXPART模型将其追溯到南部非洲和马达加斯加的生物质燃烧事件。来自ACE和MOPITT等卫星实验的数据,以及可用的臭氧探测数据,通常显示出不同数据集之间的良好一致性。

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