Dry deposition of ozone: some measurements ofdeposition velocity and of vertical profiles to 100 metres
作者： I. Colbeck , Roy M. Harrison
DOI: 10.1016/0004-6981(85)90007-1
关键词: Environmental science 、 Snow 、 Diurnal temperature variation 、 Hydrology 、 Moisture 、 Atmospheric instability 、 Anticyclone 、 Atmospheric sciences 、 Deposition (aerosol physics) 、 Ozone 、 Depot
摘要: Abstract Deposition velocities for O3 to grassland have been measured by the gradient method. Values range from 0.08 0.91 cms−1 and are shown be influenced most substantially changes in surface conditions. deposition is inhibited presence of snow or moisture at tends decrease as afternoon progresses. Vertical profiles temperature 100 m height indicative depletion dry a diminution concentration ground-level due inhibition vertical mixing aloft during periods atmospheric stability. Dry fluxes adequate account diurnal variation observed rural areas summer anticyclonic
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