Air Masses and Weather Types: A Useful Tool for Characterizing Precipitation Chemistry and Wet Deposition

被引:25
作者
Calvo, A. I. [1 ]
Pont, V. [2 ]
Olmo, F. J. [3 ,4 ]
Castro, A. [5 ]
Alados-Arboledas, L. [3 ,4 ]
Vicente, A. M. [1 ]
Fernandez-Raga, M. [5 ]
Fraile, R. [5 ]
机构
[1] Univ Aveiro, Ctr Environm & Marine Studies CESAM, P-3810193 Aveiro, Portugal
[2] Univ Toulouse 3, CNRS UPS, UMR 5560, Lab Aerol OMP, F-31400 Toulouse, France
[3] Univ Granada, CEAMA, Atmospher Phys Grp, Granada 18006, Spain
[4] Univ Granada, Dept Appl Phys, E-18071 Granada, Spain
[5] Univ Leon, IMARENAB, Dept Phys, E-24071 Leon, Spain
关键词
Rainwater chemical composition; Trajectory analysis; Circulation weather types; N deposition; Wet deposition; CHEMICAL-COMPOSITION; NITROGEN DEPOSITION; ORGANIC-ACIDS; ATMOSPHERIC DEPOSITION; RAINWATER CHEMISTRY; ACETIC-ACIDS; URBAN SITE; ANTHROPOGENIC INFLUENCES; TROPOSPHERIC OZONE; METROPOLITAN-AREA;
D O I
10.4209/aaqr.2012.03.0068
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
This study is an analysis of 344 days with rainfall recorded during five years in a remote regional background EMEP (Cooperative Programme for the Monitoring and Evaluation of the Long Range Transmission of Air Pollutants in Europe) station in Spain. The chemical composition of the rainwater associated with air masses (nine categories) and weather types (26 categories) was characterized. The chemical composition of rainwater was dominated by calcium (Ca2+) and sulphate (SO42--S), with VWM (Volume Weighted Mean) during the period studied (2002-2006), with 55 mu eq/L and 34 mu eqS/L, respectively. Calcium, sodium (Na+), ammonium (NH4+-N) and magnesium (Mg2+) seem to be dominant components in the neutralization of the rainwater. By applying Pearson correlations, principal component analysis and enrichment factors, it is possible to identify source types for the precipitation constituents. Interannual and intra-annual variability was also been studied. High calcium levels are associated with the frequent intrusions of Saharan dust that occur during the summer, and the maximums of chlorine and sodium in the winter may be due to the greater amount of maritime air recorded during this season. Wet deposition was determined by focusing on nitrogen deposition, registering mean annual values of 155 mgN/m(2)/year (from the NO3--N) and 165 mgN/m(2)/year (from the NH4+-N).
引用
收藏
页码:856 / 878
页数:23
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