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• W2093003859 abstract "Abstract Aerosols were measured with two aircraft-mounted spectrometer probes from 0.1 to 23.5 μm particle radius, between 1000 and 600 mb pressure altitude (100–4300 m MSL), and up to 200 km distance off the shores of Virginia and Bermuda. The particle size distributions, typically bimodal with modes around 0.1 μm and several μm particle radius, were integrated analytically to yield mass and number concentrations. The relatively long-lived accumulation mode, of greater importance to long-range transport of S pollutants than the shorter-lived, coarse-mode aerosol fraction, showed both horizontal and vertical variabilities. Horizontally, the atmosphere was patchy in its aerosol content from tens to hundreds of km. Vertically, the accumulation-mode mass formed three atmospheric layers: A boundary layer below 900 mb that contained 10–20 μg m −3 aerosol mass, a band between 700 and 900 mb with 2–5 μg m −3 , and a layer above 700 mb that had less than 2 μgm −3 of particles. No statistically significant differences in aerosol masses between the U.S. east coast and Bermuda could be detected within the lowest and highest atmospheric layers that were investigated. Between 700 and 900mb pressure altitudes, however, the accumulation-mode mass concentration off the Virginia coast was twice than what was measured at Bermuda. In terms of fluxes, computed from the spectrometer probe-derived masses and Loran-C-measured wind velocities, it was found that 65% of the paniculate burden leaving the U.S. east coast reached Bermuda. At Bermuda, the particulate burden reaching the islands from the west was 1.6 times the fluxes of background aerosols from the south and/or the east." @default.
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• W2093003859 date "1988-01-01" @default.
• W2093003859 modified "2023-09-26" @default.
• W2093003859 title "Aerosols over the western atlantic: Scale heights, concentrations and fluxes" @default.
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• W2093003859 doi "https://doi.org/10.1016/0004-6981(88)90469-6" @default.
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