Marinoni A, Cristofanelli P, Calzolari F, Roccato F, Bonafè U, Bonasoni P
CNR - Institute for Atmospheric Sciences and Climate, Via Gobetti 101, 40129 Bologna, Italy.
Sci Total Environ. 2008 Mar 1;391(2-3):241-51. doi: 10.1016/j.scitotenv.2007.10.004. Epub 2007 Dec 11.
Particle size distribution in the range 0.3<D(p)<or=20 microm, has been analysed from August 2002 to July 2006 at the GAW Station of Mt. Cimone (44.10 N, 10.42 E; 2165 m asl) in the northern Italian Apennines. The seasonal aerosol number size distribution, characterized by a bimodal shape, showed a behaviour typical for background conditions, characterized by highest values in summer and lowest in winter. The seasonal and diurnal variations of the larger accumulation mode (0.3<D(p)<or=1 microm average values: 26.15 cm(-3)) and the coarse mode (1<Dp<or=20 microm, average value: 0.17 cm(-3)) particle number concentrations (N 0.3-1 and N 1-20, respectively) exhibited a seasonal cycle with the highest values in spring-summer and the lowest value in autumn-winter. Except in winter, N 0.3-1 showed a clear diurnal variation with high values during day-time. N 1-20 showed a less marked diurnal variation (but with higher variability), suggesting the influence of non-continuous sources of coarse particle (i.e. Saharan dust events). Since July 2005, continuous measurement of black carbon (BC) concentrations was also available at the measurement site. On average low BC concentrations were recorded (average value: 0.28 microg m(-3)) even if a few events of high concentrations were recorded both in warm and cold season. Apart from wet scavenging processes which strongly affected aerosol concentrations, combined analysis of N 0.3-1, BC, meteorological parameters and air mass back-trajectories, suggests that the transport of polluted air masses from the lower troposphere (by local, regional or long-range transport) represents an important mechanism favouring N 0.3-1 and BC increases at Mt. Cimone. In particular, a trajectory statistical analysis for the period July 2005-July 2006 allowed the identification of the main source regions of BC and N 0.3-1 for Mt. Cimone: north Italy, west Europe and east Europe.
2002年8月至2006年7月期间,对意大利亚平宁山脉北部奇莫内山(北纬44.10度,东经10.42度;海拔2165米)全球大气观测站0.3<D(p)≤20微米范围内的粒径分布进行了分析。季节性气溶胶数浓度粒径分布呈双峰形态,表现出典型的背景条件特征,夏季值最高,冬季值最低。较大积聚模态(0.3<D(p)≤1微米,平均值:26.15厘米⁻³)和粗模态(1<Dp≤20微米,平均值:0.17厘米⁻³)的粒子数浓度(分别为N₀.₃₋₁和N₁₋₂₀)的季节和日变化呈现出季节性周期,春夏最高,秋冬最低。除冬季外,N₀.₃₋₁呈现出明显的日变化,白天值较高。N₁₋₂₀的日变化不太明显(但变异性较高),表明粗粒子非连续源(即撒哈拉沙尘事件)的影响。自2005年7月以来,测量站点还可进行黑碳(BC)浓度的连续测量。即使在温暖和寒冷季节都记录到了少数高浓度事件,但平均记录到的BC浓度较低(平均值:0.28微克/立方米)。除了对气溶胶浓度有强烈影响的湿清除过程外,对N₀.₃₋₁、BC、气象参数和空气团后向轨迹的综合分析表明,来自对流层下部的污染空气团的输送(通过本地、区域或长距离输送)是奇莫内山N₀.₃₋₁和BC增加的一个重要机制。特别是,对2005年7月至2006年7月期间的轨迹统计分析确定了奇莫内山BC和N₀.₃₋₁的主要源区:意大利北部、西欧和东欧。