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• W2912698761 abstract "During the first Intensive Observation Period (IOP1) of the SHADOW (SaHAran Dust Over West Africa) campaign carried out during March–June 2015, the Mbour site (Senegal) was reinforced with a large setup of in-situ and remote sensing instruments to measure the aerosol optical, physical and chemical properties as well as the atmospheric dynamical features over the site. Here, we use this dataset to study the impact of Sea Breeze (SB) on the aerosol properties. Two case studies were selected: (i) one representative of SB events observed during typical Harmattan conditions, (ii) and one representative of SB events observed during a Harmattan desert dust event. Both cases show a strong influence of the SB period on the dry Mass Scattering Efficiency (MSE), which increases by a factor of up to 1.4. Given the fact that SB occurred every other day at this coastal site during IOP1 (dry season) and that the relative humidity may reach 96%, the effect of such event on the radiative forcing may not be negligible. In order to evaluate the effects of different flows on aerosol transport, recirculation and stagnation factors were retrieved from wind components. The air mass recirculation factor implies that aerosols previously transported from the land over the sea are then brought back inland. In both cases, high recirculation factors were calculated (between 0.84 and 0.98) and air mass stagnation was observed right before the SB establishment. However, this stagnation is observed over the sea during the first case while it is located near the coast during the second case, which has a significant impact on the aerosol evolution. Indeed, a stagnation of air masses over the sea is associated with an increase in fine aerosol mass concentrations (PM1, PM2.5) due to a higher contribution of marine and anthropogenic sources notably for organic aerosols, and a higher contribution of more-oxidized organics. This contribution is lower when the air mass stagnation occurs over the shoreline during the desert dust event." @default.
• W2912698761 created "2019-02-21" @default.
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• W2912698761 date "2019-04-01" @default.
• W2912698761 modified "2023-10-11" @default.
• W2912698761 title "Aerosol variability induced by atmospheric dynamics in a coastal area of Senegal, North-Western Africa" @default.
• W2912698761 cites W1162407187 @default.
• W2912698761 cites W1183314382 @default.
• W2912698761 cites W1506566217 @default.
• W2912698761 cites W1593263354 @default.
• W2912698761 cites W1918776395 @default.
• W2912698761 cites W1967717552 @default.
• W2912698761 cites W1968805615 @default.
• W2912698761 cites W1969298331 @default.
• W2912698761 cites W1970370142 @default.
• W2912698761 cites W1976129559 @default.
• W2912698761 cites W1980054906 @default.
• W2912698761 cites W1982732147 @default.
• W2912698761 cites W1996330583 @default.
• W2912698761 cites W1998373198 @default.
• W2912698761 cites W2000058464 @default.
• W2912698761 cites W2000395827 @default.
• W2912698761 cites W2001349167 @default.
• W2912698761 cites W2004860873 @default.
• W2912698761 cites W2005192947 @default.
• W2912698761 cites W2014902034 @default.
• W2912698761 cites W2015813609 @default.
• W2912698761 cites W2025547443 @default.
• W2912698761 cites W2031847508 @default.
• W2912698761 cites W2033819401 @default.
• W2912698761 cites W2040129659 @default.
• W2912698761 cites W2056981114 @default.
• W2912698761 cites W2057802876 @default.
• W2912698761 cites W2059745395 @default.
• W2912698761 cites W2060355556 @default.
• W2912698761 cites W2065403651 @default.
• W2912698761 cites W2065438566 @default.
• W2912698761 cites W2073270114 @default.
• W2912698761 cites W2076101960 @default.
• W2912698761 cites W2077892038 @default.
• W2912698761 cites W2079896519 @default.
• W2912698761 cites W2082288933 @default.
• W2912698761 cites W2084591555 @default.
• W2912698761 cites W2084701612 @default.
• W2912698761 cites W2084777698 @default.
• W2912698761 cites W2090996783 @default.
• W2912698761 cites W2094037082 @default.
• W2912698761 cites W2094408786 @default.
• W2912698761 cites W2104027902 @default.
• W2912698761 cites W2118055455 @default.
• W2912698761 cites W2121498382 @default.
• W2912698761 cites W2135327496 @default.
• W2912698761 cites W2137395270 @default.
• W2912698761 cites W2138088023 @default.
• W2912698761 cites W2139734571 @default.
• W2912698761 cites W2142656089 @default.
• W2912698761 cites W2143058944 @default.
• W2912698761 cites W2157451705 @default.
• W2912698761 cites W2163559599 @default.
• W2912698761 cites W2163922819 @default.
• W2912698761 cites W2164231461 @default.
• W2912698761 cites W2166543245 @default.
• W2912698761 cites W2168466445 @default.
• W2912698761 cites W2173616934 @default.
• W2912698761 cites W2175681596 @default.
• W2912698761 cites W2176179542 @default.
• W2912698761 cites W2176619265 @default.
• W2912698761 cites W2178269757 @default.
• W2912698761 cites W2304530970 @default.
• W2912698761 cites W2308728425 @default.
• W2912698761 cites W2319076967 @default.
• W2912698761 cites W2347063623 @default.
• W2912698761 cites W2406260245 @default.
• W2912698761 cites W2411234785 @default.
• W2912698761 cites W2502777608 @default.
• W2912698761 cites W2565325021 @default.
• W2912698761 cites W2567098959 @default.
• W2912698761 cites W2594074802 @default.
• W2912698761 cites W2601941415 @default.
• W2912698761 cites W2708567945 @default.
• W2912698761 cites W2764298000 @default.
• W2912698761 cites W353030162 @default.
• W2912698761 doi "https://doi.org/10.1016/j.atmosenv.2019.01.041" @default.
• W2912698761 hasPublicationYear "2019" @default.
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