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One-year observations of the vertical structure of Saharan dust over Athens, Greece monitored by NTUA's lidar system in the frame of EARLINET

机译:雅典纵横膜纵向结构的一年观察,在耳环框架中被NTUA激光雷达系统监测的希腊

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Suspended aerosol particles play a significant role in the Global Change issue. Every year huge quantities of Saharan dust are transported to the European continent and North Atlantic Sea. Since May 1, 2000, an elastic backscatter lidar station is in operation in Athens, Greece, in the frame of the European LIDAR Network (EARLINET), aiming at the monitoring of extreme aerosol events over the Eastern Mediterranean Sea. During the first year of operation 20 cases of Saharan dust transport to the East Mediterranean Sea (EMS), were successfully observed. The lidar data are correlated with meteorological and satellite observations, including the aerosol index (AI) data from the Total Ozone Mapping Spectrometer (TOMS) and the SeaWiFS satellite images. The analysis of the data collected so far, made possible a first statistical approach of the vertical and horizontal extent and of the seasonal variation of free tropospheric Saharan dust layers over the EMS area. The main results of this work are: i) multiple dust layers of variable thickness (0.5-4 km) are systematically observed in the altitude region 2-6 km, ii) Saharan dust outbreaks take place all year round, with more pronounced frequencies during the summer period and can persist for a few days (1-5), iii) 24-48 hours are usually needed for the Saharan air masses to reach the EMS area, and finally iv) the TOMS AI values can reach 1.5-3.5 over Greece. These lidar data gave the aerosol vertical structure over the Eastern Mediterranean Sea during Saharan dust outbreaks and can be a direct input for global radiative transfer models.
机译:悬浮气溶胶颗粒在全球变革问题中发挥着重要作用。每年都有大量的撒哈拉尘埃被运送到欧洲大陆和北大西洋海。自2000年5月1日起,弹性反向散射赛车站在雅典,希腊雅典,欧洲连日星网络(Earlinet)的框架中,旨在监测东部地中海的极端气溶胶事件。在运作的第一年,成功地观察到东地中海(EMS)的第一次撒哈拉粉尘运输。 LIDAR数据与气象和卫星观察相关,包括来自总臭氧映射光谱仪(TOMS)和SeaWIFS卫星图像的气溶胶指数(AI)数据。到目前为止所收集的数据分析,使得垂直和水平范围的第一种统计方法和EMS区域上自由的对流层撒哈拉尘层的季节变化。这项工作的主要结果是:i)在海拔地区2-6km,II)撒哈拉尘埃爆发的多年来,多年来,在系统地观察到多个可变厚度(0.5-4 km)的多种灰尘层,在全年举行,均为更明显的频率夏季,可以持续几天(1-5),iii)24-48小时通常需要撒哈拉空气群众达到EMS地区,最后IV)汤姆斯AI值可以达到1.5-3.5希腊。这些激光乐队数据在撒哈拉尘埃爆发期间在东部地中海提供了气溶胶垂直结构,可以是全球辐射转移模型的直接输入。

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