Flocas Helena A, Assimakopoulos Vasiliki D, Helmis Costas G
Department of Applied Physics, Faculty of Physics, University of Athens, Building PHYS-5, University campus, 157 84 Athens, Greece.
Sci Total Environ. 2006 Aug 31;367(2-3):872-87. doi: 10.1016/j.scitotenv.2005.12.028. Epub 2006 Feb 28.
In this study an attempt is made to investigate the aerosol spatial and size distributions at different heights over the Greater Athens Area (GAA), Greece, under sea breeze conditions and clear sky and to further discuss possible implications for aerosol characteristics. The data used are airborne measurements of aerosol collected during two flights that were performed within the context of the 1997 STAAARTE experimental campaign. The aerosol measurements cover particle diameters from 0.1 to 45.5 microm. The horizontal and vertical distribution revealed that higher concentrations exist within or just above the atmospheric boundary layer, while greater concentrations are observed over the sea compared to land at high altitudes. At all altitudes the number size distributions show dominant diameter ranges between 0.1 and 0.3 microm at all altitudes. The volume distributions are characterised by two modes, one in the accumulation and the other in the coarse particle regime. At lower altitudes, fresh combustion emissions more likely cause the predominance of the size range 0.1-0.3 microm while enhanced physical and chemical processes that favour the growth of smaller particles to larger sizes could also act. The relative humidity does not seem to affect the observed number size distributions at low altitudes, where relative humidity is below 70% while at 4000 m the distributions seem to change over the sea where the humidity increases.
在本研究中,我们试图调查希腊大雅典地区(GAA)在海风条件和晴空下不同高度处的气溶胶空间分布和粒径分布,并进一步讨论其对气溶胶特性的可能影响。所使用的数据是在1997年STAAARTE实验活动中进行的两次飞行期间收集的气溶胶机载测量数据。气溶胶测量涵盖的粒径范围为0.1至45.5微米。水平和垂直分布表明,较高浓度存在于大气边界层内或其上方,而在高海拔地区,与陆地相比,海上观测到的浓度更高。在所有高度上,数量粒径分布显示在所有高度上主导粒径范围在0.1至0.3微米之间。体积分布具有两种模式,一种在积聚模式,另一种在粗颗粒模式。在较低高度,新鲜燃烧排放更有可能导致0.1 - 0.3微米粒径范围占主导,而有利于较小颗粒生长为较大颗粒的增强物理和化学过程也可能起作用。相对湿度似乎不会影响低海拔处观测到的数量粒径分布,低海拔处相对湿度低于70%,而在4000米高度,在湿度增加的海域,分布似乎会发生变化。