Aerosols in Northern Morocco: Input pathways and their chemical fingerprint

被引:22
作者
Benchrif, A. [1 ]
Guinot, B. [2 ]
Bounakhla, M. [1 ]
Cachier, H. [3 ]
Damnati, B. [4 ]
Baghdad, B. [5 ]
机构
[1] Ctr Natl Energie Sci & Tech Nucl, Rabat, Morocco
[2] Univ Toulouse, CNRS, Lab Aerol, UPS, Toulouse, France
[3] Lab Sci Climat & Environm, Gif Sur Yvette, France
[4] Fac Sci & Technol, Tanger, Morocco
[5] Inst Agron & Vet, Rabat, Morocco
关键词
Aerosols; PM2.5; Western Mediterranean Basin; Chemical composition; Back trajectory clustering; Maritime traffic; EASTERN MEDITERRANEAN SEA; SHIP EMISSIONS; MASS CLOSURE; VARIABILITY; SUMMERTIME; BASIN; CAMPAIGN; CLIMATE; IMPACT;
D O I
10.1016/j.atmosenv.2017.11.047
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The Mediterranean basin is one of the most sensitive regions in the world regarding climate change and air quality. Deserts and marine aerosols combine with combustion aerosols from maritime traffic, large urban centers, and at a larger scale from populated industrialized regions in Europe. From Tetouan city located in the North of Morocco, we attempted to better figure out the main aerosol transport pathways and their respective aerosol load and chemical profile by examining air mass back trajectory patterns and aerosol chemical compositions from May 2011 to April 2012. The back trajectory analysis throughout the sampling period led to four clusters, for which meteorological conditions and aerosol chemical characteristics have been investigated. The most frequent cluster (CL3: 39%) corresponds to polluted air masses coming from the Mediterranean Basin, characterized by urban and marine vessels emissions out of Spain and of Northern Africa. Two other polluted clusters were characterized. One is of local origin (CL1: 22%), with a marked contribution from urban aerosols (Rabat, Casablanca) and from biomass burning aerosols. The second (CL2: 32%) defines air masses from the near Atlantic Ocean, affected by pollutants emitted from the Iberian coast. A fourth cluster (CL4: 7%) is characterized by rather clean, fast and rainy oceanic air masses, influenced during their last 24 h before reaching Tetouan by similar sources with those affecting CL2, but to a lesser extent. The chemical data show that carbonaceous species are found in the fine aerosols fraction and are generally from local primary sources (low OC/EC) rather than long-range transported. In addition to fresh traffic and maritime vessel aerosols, our results suggest the contribution of local biomass burning.
引用
收藏
页码:140 / 147
页数:8
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