1979
DOI: 10.1016/0004-6981(79)90001-5
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First European community Campaign for remote sensing of atmospheric pollution, LACQ (France), 7–11 July 1975

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Cited by 16 publications
(4 citation statements)
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“…plume as a tracer of opportunity of the lower atmosphere, it was possible to track the daily evolution of the wind field and the dispersive conditions (as previously performed in other experiments in different regions, Millán et al, 1979;Guillot et al, 1979;Chung et al, 1981;Hoff et al, 1982;Portelli, 1982;Millán et al, 1987;Eastman et al, 1995;Palau, 2003).…”
Section: Methodsmentioning
confidence: 96%
“…plume as a tracer of opportunity of the lower atmosphere, it was possible to track the daily evolution of the wind field and the dispersive conditions (as previously performed in other experiments in different regions, Millán et al, 1979;Guillot et al, 1979;Chung et al, 1981;Hoff et al, 1982;Portelli, 1982;Millán et al, 1987;Eastman et al, 1995;Palau, 2003).…”
Section: Methodsmentioning
confidence: 96%
“…Besides, by using the plume transport direction aloft as a tracer of opportunity of the wind field at the plume (air pollutants) transport height, it is possible to identify the diurnal advective regimes in the mid-troposphere. Previous studies in different climatological and geographical regions have already used plume transport directions aloft to track the main dispersive characteristics and daily evolution of the windfield at the plume transport height (Millán, 1979;Guillot et al, 1979;Chung et al, 1981;Hoff et al, 1982;Portelli, 1982;Millán et al, 1987;Eastman et al, 1995;Palau et al, 2005). This availability of measurements aloft, obtained by means of a vehicle equipped with a COSPEC remote sensor, represents a clear advantage over the information provided by the fixed ground-level monitoring stations for atmospheric pollutant control, especially on mid-latitude complex terrain (where vertical wind directional shear is the most persistent pattern).…”
Section: Acpdmentioning
confidence: 99%
“…Measurements were taken throughout the day to record any changes that might occur in the plume transport direction or in the dispersive conditions. Thus, using this plume as a tracer of opportunity of the lower atmosphere, it was possible to track the daily evolution of the wind field and the dispersive conditions (as previously performed in other experiments in different regions, Millán et al, 1979;Guillot et al, 1979;Chung et al, 1981;Hoff et al, 1982;Portelli, 1982;Millán et al, 1987;Eastman et al, 1995;Palau, 2003).…”
Section: Methodsmentioning
confidence: 97%