1982
DOI: 10.1016/0004-6981(82)90448-6
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Some observations of the influence of meteorological variables on the size distribution of natural aerosol particles

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Cited by 16 publications
(7 citation statements)
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“…They provide reasonable predictions for extinction over the open ocean, continental or desert environments, but in coastal regions their reliability is less [19][20][21] when, due to onshore winds, sea spray aerosols become mixed with continental aerosols. Thus, size distribution of atmospheric aerosols strongly depends on the sources and sinks as well as the meteorological processes acting during their lifetime [22][23] , on the type and history of the airmass, as well as on the boundary-layer circulation (like land-and sea-breezes that occur daily in coastal areas) [24][25] .…”
Section: Introductionmentioning
confidence: 99%
“…They provide reasonable predictions for extinction over the open ocean, continental or desert environments, but in coastal regions their reliability is less [19][20][21] when, due to onshore winds, sea spray aerosols become mixed with continental aerosols. Thus, size distribution of atmospheric aerosols strongly depends on the sources and sinks as well as the meteorological processes acting during their lifetime [22][23] , on the type and history of the airmass, as well as on the boundary-layer circulation (like land-and sea-breezes that occur daily in coastal areas) [24][25] .…”
Section: Introductionmentioning
confidence: 99%
“…This presumably reflects the pollution from the heavily industrialized Midlands about 150 km south of Manchester. Choularton et al (1982) have reported that the highest concentrations of 0.7-1.4 pm particles occurred at Manchester when the airmass had traversed the Midlands.…”
Section: Resultsmentioning
confidence: 99%
“…Choularton et al (1982) have demonstrated that, in a stratified atmosphere typical of stable atmospheric conditions (Richardson number Ri ) 0), more of the larger particles () 0.3 ~ in diameter) are removed by gravitational settling. Choularton et al (1982) have demonstrated that, in a stratified atmosphere typical of stable atmospheric conditions (Richardson number Ri ) 0), more of the larger particles () 0.3 ~ in diameter) are removed by gravitational settling.…”
Section: Atmospheric Trace-element Scavengingmentioning
confidence: 99%