首页> 外文期刊>Tellus, Series B. Chemical and Physical Meteorology >Clear-sky closure studies of lower tropospheric aerosol and water vapor during ACE-2 using airborne sunphotometer, airborne in-situ, space-borne, and ground-based measurements
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Clear-sky closure studies of lower tropospheric aerosol and water vapor during ACE-2 using airborne sunphotometer, airborne in-situ, space-borne, and ground-based measurements

机译:使用机载日光光度计,机载就地,星载和地面测量,对ACE-2期间对流层下层气溶胶和水蒸气的晴空封闭研究

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摘要

We report on clear-sky column closure experiments (CLEARCOLUMN) performed in the Canary Islands during the second Aerosol Characterization Experiment (ACE-2) in June/July 1997. We present CLEARCOLUMN results obtained by combining ariborne sunphotometer and in-situ (optical particle counter, nephelometer, and absorption photometer) measurements taken aboard the Pelican aircraft, space-borne NOAA/AVHRR data and ground-based lidar and sunphotometer measurements. During both days discussed here, vertical profiles flown in cloud-free air masses revealed 3 distinctly different layers: a marine boundary layer (MBL) with varying pollution levels, and elevated dust layer, and a very clean layer between the MBL and the dust layer. A key result of this study is the achievement of closure between extinction or layer aerosol optical depth (AOD) computed from continuous in-situ aerosol size-distributions and composition and those measured with the airborne sunphotometer. In the dust, the agreement in layer AOD (λ = 380-1060 nm) is 3-8%. In the MBL there is a tendency for the in-situ results to be slightly lower than the sunphotometer measurements (10-17% at λ = 525 nm), but these differences are within the combined error bars of the measurements and computations.
机译:我们报告了1997年6月/ 7月在加那利群岛进行的第二次气溶胶表征实验(ACE-2)期间进行的晴空柱封闭实验(CLEARCOLUMN)。计数器,浊度计和吸收光度计)测量值,在Pelican飞机上进行,星载NOAA / AVHRR数据以及地面激光雷达和日光计测量值。在这里讨论的两天中,在无云的空气团中飞行的垂直剖面显示出3个明显不同的层:具有不同污染水平的海洋边界层(MBL),高扬尘层以及MBL和尘埃层之间的非常干净的层。这项研究的关键结果是,根据连续的原位气溶胶粒径分布和组成与使用机载日光光度计测量的结果,得出了消光或层气溶胶光学深度(AOD)之间的闭合效果。在粉尘中,AOD层(λ= 380-1060 nm)中的一致性为3-8%。在MBL中,原位结果倾向于比日光光度计的测量值稍低(在λ= 525 nm时为10-17%),但是这些差异在测量和计算的组合误差范围内。

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