Arid
DOI10.1016/j.atmosenv.2016.06.041
Long-range transport of Saharan dust and chemical transformations over the Eastern Mediterranean
Athanasopoulou, E.1,2; Protonotariou, A.1; Papangelis, G.1; Tombrou, M.1; Mihalopoulos, N.2; Gerasopoulos, E.2
通讯作者Athanasopoulou, E.
来源期刊ATMOSPHERIC ENVIRONMENT
ISSN1352-2310
EISSN1873-2844
出版年2016
卷号140页码:592-604
英文摘要

Three recent Saharan dust outbreaks during different seasons (4-6 days in winter of 2009, late autumn of 2010 and summer of 2011) are selected in order to study the chemical footprint and aging processes of dust intrusions over the Eastern Mediterranean (EM). The applied model system (PMCAMx, WRF and GEOS-CHEM) and methodology are found competent to reproduce dust production, long-range transport and chemical transformations over the EM, with the synergistic use of synoptic patterns analysis, optical depth retrievals, back-trajectories, surface and satellite aerosol measurements. The dust loads were high during the cold period events and much lighter during summertime, when transport was mainly in the free troposphere. In all cases, dust originated from the northwest and/or west Saharan desert and reached the EM from the west/southwest. Sensitivity runs underlie the effect of dust transport on the chemical constituents of aerosols over the EM and show a large impact on calcium (70-90% of maximum daily values 2-5 mu g m(-3)), with its gradient at surface level being around -10% per 100 km along the dust pathway. For the cold period cases, this value can also be considered analogous to the dust dissipation ratio, because the plume is vertically extended down to the surface layers. Interestingly, the surface particulate nitrate concentrations over the EM are reversely affected by the approaching dust loads, exhibiting the highest values (up to 6 mu g m(-3)) and the largest dust fraction (ca. 70%) during summertime. This is attributed to the enhanced nitric acid formation under high atmospheric temperature and insolation, its uptake onto the carbonate dust particles, and their effective accumulation, due to low deposition rates over the sea and scarce precipitation. Sulfate formation onto dust particles is found insignificant (rapid reaction with ammonia and/or sea-salt), while the influence of dust and sea-salt on sodium, when spatio-temporal averages are calculated, is approximately equal. (C) 2016 Elsevier Ltd. All rights reserved.


英文关键词Saharan dust events Eastern Mediterranean (EM) Aerosol modeling Chemical impacts of dust Dust-bound nitrate
类型Article
语种英语
国家Greece
收录类别SCI-E
WOS记录号WOS:000380083200054
WOS关键词CONTAINING MINERAL DUST ; AIR-QUALITY ; HETEROGENEOUS CHEMISTRY ; ATMOSPHERIC CHEMISTRY ; PARTICULATE MATTER ; MODEL DESCRIPTION ; NORTH-ATLANTIC ; AEROSOL ; ATHENS ; EMISSIONS
WOS类目Environmental Sciences ; Meteorology & Atmospheric Sciences
WOS研究方向Environmental Sciences & Ecology ; Meteorology & Atmospheric Sciences
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/191610
作者单位1.Univ Athens, Dept Appl Phys, Athens 15784, Greece;
2.Natl Observ Athens, Inst Environm Res & Sustainable Dev, Athens 15236, Greece
推荐引用方式
GB/T 7714
Athanasopoulou, E.,Protonotariou, A.,Papangelis, G.,et al. Long-range transport of Saharan dust and chemical transformations over the Eastern Mediterranean[J],2016,140:592-604.
APA Athanasopoulou, E.,Protonotariou, A.,Papangelis, G.,Tombrou, M.,Mihalopoulos, N.,&Gerasopoulos, E..(2016).Long-range transport of Saharan dust and chemical transformations over the Eastern Mediterranean.ATMOSPHERIC ENVIRONMENT,140,592-604.
MLA Athanasopoulou, E.,et al."Long-range transport of Saharan dust and chemical transformations over the Eastern Mediterranean".ATMOSPHERIC ENVIRONMENT 140(2016):592-604.
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