Atmospheric Chemistry and Physics www.atmos-chem-phys.net 1680-7316 1680-7324 8 20 2008 10.5194/acp-8-6245-2008 http://www.atmos-chem-phys.net/8/6245/2008/ http://www.atmos-chem-phys.net/8/6245/2008/acp-8-6245-2008.html http://www.atmos-chem-phys.net/8/6245/2008/acp-8-6245-2008.pdf 6245 6259 2008-10-28 Attenuation of concentration fluctuations of water vapor and other trace gases in turbulent tube flow W. J. Massman wmassman@fs.fed.us A. Ibrom US Forest Service, Rocky Mountain Research Station, 240 West Prospect, Fort Collins, CO 80526, USA Bio Systems Department, Risø National Laboratory, DTU, Frederiksborgvej, 4000 Roskilde, Denmark Recent studies with closed-path eddy covariance (EC) systems have indicated that the attenuation of fluctuations of water vapor concentration is dependent upon ambient relative humidity, presumably due to sorption/desorption of water molecules at the interior surface of the tube. Previous studies of EC-related tube attenuation effects have either not considered this issue at all or have only examined it superficially. Nonetheless, the attenuation of water vapor fluctuations is clearly much greater than might be expected from a passive tracer in turbulent tube flow. This study reexamines the turbulent tube flow issue for both passive and sorbing tracers with the intent of developing a physically-based semi-empirical model that describes the attenuation associated with water vapor fluctuations. Toward this end, we develop a new model of tube flow dynamics (radial profiles of the turbulent diffusivity and tube airstream velocity). We compare our new passive-tracer formulation with previous formulations in a systematic and unified way in order to assess how sensitive the passive-tracer results depend on fundamental modeling assumptions. 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