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Multiyear aerosol observations with dual-wavelength Raman lidar in the framework of EARLINET

机译:在EaRLINET框架内使用双波长拉曼激光雷达进行多年气溶胶观测

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摘要

For the first time, a Raman lidar operating simultaneously in the ultraviolet (UV) and in the visible wavelength range was employed to measure vertical profiles of volume extinction coefficients of particles at 355 and 532 nm, the respective Angstromngstrom exponent, and the 355-nm and 532-nm extinction-to-backscatter ratio ( lidar ratio) on a routine basis for several years. The long-term observations were performed at Leipzig (52degreesN, 12degreesE), Germany, in the framework of the European Aerosol Research Lidar Network (EARLINET) project from May 2000 to March 2003. The lidar data were acquired under nighttime conditions. The main findings describe the mean optical properties of central European haze ( anthropogenic particles) and can be summarized as follows. The 3-year mean, planetary boundary layer (PBL) extinction coefficients were 191 Mm(-1) at 355 nm and 94 Mm(-1) at 532 nm. The respective mean Angstromngstrom exponent (for the 355-532-nm wavelength range) was 1.4 in the upper PBL (above 1000 m). The PBL stretched, on average, to heights of 1300 m ( winter) and 2350 m (summer). PBL mean particle optical depths were 0.38 (355 nm, +/-0.23 standard deviation) and 0.18 (532 nm, +/-0.11 standard deviation). Free tropospheric particles contributed 2% (clean free troposphere) to 88% ( major Saharan dust events) to the tropospheric optical depth. The average was 17% (355 nm) and 22% (532 nm) in 2000-2003. Angstromngstrom exponents in the free troposphere of about one reflect the dominant influence of Saharan dust and aged smoke on the optical properties in this height range. Three-year mean lidar ratios of 58 sr (355 nm) and 53 sr ( 532 nm) were found in the upper part of the PBL. Free tropospheric lidar ratios were on average 52 sr ( 355 nm) and 53 sr ( 532 nm). From combined observations with the Aerosol Robotic Network (AERONET) Sun photometer and the EARLINET lidar, extinction-to-backscatter ratios at 1064 nm were estimated to be, on average, 45 sr. A comparison with optical measurements made at the Leipzig University from 1990 to 1994 indicates that the PBL extinction coefficient at 532 nm decreased by a factor of about 2 (summer half year) to almost 5 (winter season) since the unification of Germany (1990), mainly caused by the industrial breakdown in eastern Germany in the early 1990s.
机译:首次使用拉曼激光雷达同时在紫外线(UV)和可见光波长范围内操作,以测量355和532 nm粒子的体积消光系数,相应的埃指数和355 nm的垂直消光系数的垂直分布和532 nm的消光/背向散射比(激光雷达比),历时数年。在2000年5月至2003年3月的欧洲气溶胶研究激光雷达网络(EARLINET)项目的框架内,在德国莱比锡(52°N,12°E)进行了长期观测。激光雷达数据是在夜间条件下采集的。主要发现描述了中欧雾霾(人为颗粒)的平均光学性质,可以归纳如下。 3年平均行星边界层(PBL)的消光系数在355 nm处为191 Mm(-1),在532 nm处为94 Mm(-1)。在较高的PBL(1000 m以上)中,相应的平均埃指数(在355-532 nm波长范围内)为1.4。 PBL平均伸展至1300 m(冬季)和2350 m(夏季)的高度。 PBL平均粒子光学深度为0.38(355 nm,标准偏差+/- 0.23)和0.18(532 nm,标准偏差+/- 0.11)。自由对流层粒子对流层光学深度贡献了2%(干净的自由对流层)到88%(主要的撒哈拉尘埃事件)。在2000-2003年,平均值为17%(355 nm)和22%(532 nm)。自由对流层的埃指数约为1,反映了该高度范围内撒哈拉尘埃和老烟对光学性能的主要影响。在PBL的上部发现了三年平均激光雷达比分别为58 sr(355 nm)和53 sr(532 nm)。自由对流层激光雷达比平均为52 sr(355 nm)和53 sr(532 nm)。通过结合使用Aerosol机器人网络(AERONET)太阳光度计和EARLINET激光雷达的观察,估计在1064 nm处的消光与背向散射比平均为45 sr。与1990年至1994年在莱比锡大学进行的光学测量结果进行的比较表明,自德国统一(1990年)以来,PBL在532 nm处的消光系数下降了约2(半年度)至近5(冬季)。主要原因是1990年代初德国东部的工业崩溃。

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