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Complex vertical layering and mixing of aerosols over the eastern Mediterranean: Active and passive remote sensing at the Cyprus University of Technology

机译:Complex vertical layering and mixing of aerosols over the eastern Mediterranean: Active and passive remote sensing at the Cyprus University of Technology

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Aerosols can have a complicated influence on climate conditions, directly as well as indirectly via cloud formation. The southeastern Mediterranean region can be characterized as a cross road of aerosols originating from European, Asian and African continents. Complex vertical aerosol distributions are frequently detected over Cyprus by means of active remote sensing. Observations of such complex aerosol layering and comparison of the measurements with aerosol products of regional and global atmospheric transport models are required to improve our understanding of life cycles of aerosol mixtures and their impact on climate as well as on satellite remote sensing products. In this study, a case of an intense desert dust outbreak from Syria and Saudi Arabia towards the eastern Mediterranean in September 2011 is presented. The observations used in this study were performed with a 532-nm polarization Lidar and a sun/sky AERONET photometer operated at 8 channels from 340 to 1640 nm wavelength. Both instruments belong to remote sensing station of the Cyprus Technical University at Limassol, Cyprus (34°N, 33°E). The lofted dust plume was doped with air masses that crossed sources of biomass burning smoke and anthropogenic pollution. In addition, the shallow marine boundary layer over the Mediterranean Sea and over Limassol became mixed with the anthropogenic haze by sea breeze circulations. The case study demonstrates the potential of combined lidar/photometer observations to deliver detailed vertically resolved information of the aerosol characteristics in terms of particle optical and microphysical properties, separately for the spherical particle fraction as well as for the non-spherical aerosol mode.
机译:气溶胶可以直接或间接地通过云的形成对气候条件产生复杂的影响。地中海东南部地区可以被描述为来自欧洲、亚洲和非洲大陆的气溶胶的交叉地带。塞浦路斯上空经常通过主动遥感探测到复杂的气溶胶垂直分布。为了更好地理解气溶胶混合物的生命周期及其对气候和卫星遥感产品的影响,需要对这种复杂的气溶胶分层进行观测,并将测量结果与区域和全球大气传输模型的气溶胶产品进行比较。在这项研究中,介绍了2011年9月从叙利亚和沙特阿拉伯向东地中海地区爆发的一次强烈沙漠沙尘暴发。本研究中使用的观测是使用532 nm偏振激光雷达和太阳/天空AERONET光度计在340至1640 nm波长的8个通道上进行的。这两台仪器都属于塞浦路斯理工大学位于塞浦路斯利马索尔的遥感站(北纬34度,东经33度)。飘浮的尘柱中掺杂了穿过生物质燃烧烟雾和人为污染源的气团。此外,地中海和利马索尔上空的浅海边界层通过海风环流与人为薄雾混合。该案例研究表明,激光雷达/光度计组合观测有可能提供颗粒光学和微物理特性方面气溶胶特性的详细垂直分辨率信息,分别适用于球形颗粒分数和非球形气溶胶模式。

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