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Measurement of tropospheric aerosol in Sao Paulo area using a new upgraded Raman LIDAR system

机译:使用新升级的拉曼激光雷达系统测量圣保罗地区对流层气溶胶

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Elastic backscatter LIDAR systems have been used to determine aerosol profile concentration in several areas such as weather, pollution and air quality monitoring. In order to determine the aerosol extinction and backscattering profiles, the Klett inversion method is largely used, but this method suffers from lack of information since there are two unknown variables to be determined using only one measured LIDAR signal, and assumption of the LIDAR ratio (the relation between the extinction and backscattering coefficients) is needed.When a Raman LIDAR system is used, the inelastic backscattering signal is affected by aerosol extinction but not by aerosol backscatter, which allows this LIDAR to uniquely determine extinction and backscattering coefficients without any assumptions or any collocated instruments. The MSP-LIDAR system, set-up in a highly dense suburban area in the city of Sao Paulo, has been upgraded to a Raman LIDAR, and in its actual 6-channel configuration allows it to monitor elastic backscatter at 355 and 532 nm together with nitrogen and water vapor Raman backscatters at 387nm and 608 nm and 408nm and 660 nm, respectively. Thus, the measurements of aerosol backscattering, extinction coefficients and water vapor mixing ratio in the Planetary Boundary Layer (PBL) are becoming available. The system will provide the important meteorological parameters such as Aerosol Optical Depth (AOD) and will be used for the study of aerosol variations in lower troposphere over the city of Sao Paulo, air quality monitoring and for estimation of humidity impact on the aerosol optical properties, without any a priori assumption. This study will present the first results obtained with this upgraded LIDAR system, demonstrating the high quality of obtained aerosol and water vapor data. For that purpose, we compared the data obtained with the new MSP-Raman LIDAR with a mobile Raman LIDAR collocated at the Center for Lasers and Applications, Nuclear and Energy Research Institute in Sao Paulo and radiosonde data from Campo de Marte Airport, in Sao Paulo.
机译:弹性后向散射激光雷达系统已用于确定几个区域的气溶胶剖面浓度,例如天气,污染和空气质量监测。为了确定气溶胶的消光和反向散射特征,大量使用了Klett反演方法,但是该方法缺乏信息,因为仅使用一个测得的LIDAR信号并假设LIDAR比率即可确定两个未知变量(当使用拉曼激光雷达系统时,非弹性后向散射信号受气溶胶消光影响,但不受气溶胶向后散射影响,这使得该激光雷达无需任何假设或任何条件即可唯一确定消光和后向散射系数。任何并置的乐器。 MSP-LIDAR系统在圣保罗市的一个高密度郊区安装,已升级为拉曼激光雷达,并以其实际的6通道配置使其可以同时监视355和532 nm的弹性反向散射分别具有387nm和608nm,408nm和660nm的氮和水蒸气拉曼背散射。因此,行星边界层(PBL)中的气溶胶反向散射,消光系数和水蒸气混合比的测量变得可用。该系统将提供重要的气象参数,例如气溶胶光学深度(AOD),并将用于研究圣保罗市对流层下层的气溶胶变化,空气质量监测以及评估湿度对气溶胶光学特性的影响。 ,无需任何先验假设。这项研究将展示使用升级后的激光雷达系统获得的首批结果,证明了所获得的气溶胶和水蒸气数据的高质量。为此,我们将新的MSP-拉曼激光雷达与移动拉曼激光雷达获得的数据进行了比较,该移动拉曼激光雷达位于圣保罗核能研究所的激光和应用中心,并与圣保罗坎普·德·马特机场的无线电探空仪数据进行了比较。 。

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