Please use this identifier to cite or link to this item: http://hdl.handle.net/11455/68137
DC FieldValueLanguage
dc.contributor.authorTsai, J.L.en_US
dc.contributor.authorChen, C.L.en_US
dc.contributor.authorTsuang, B.J.en_US
dc.contributor.authorKuo, P.H.en_US
dc.contributor.authorTseng, K.H.en_US
dc.contributor.authorHsu, T.F.en_US
dc.contributor.authorSheu, B.H.en_US
dc.contributor.authorLiu, C.P.en_US
dc.contributor.authorHsueh, M.T.en_US
dc.date2010zh_TW
dc.date.accessioned2014-06-11T05:56:18Z-
dc.date.available2014-06-11T05:56:18Z-
dc.identifier.issn1352-2310zh_TW
dc.identifier.urihttp://hdl.handle.net/11455/68137-
dc.description.abstractA 60-m flux tower was built on a 2100 m mountain for the measurement of the air pollutant concentration and the evaluation of dry deposition velocity in Central Taiwan. The tower was constructed in an evergreen broadleaf forest, which is the dominant species of forest in the world. Multiple-level SO2 concentrations and meteorological variables at the site were measured from February to April 2008. The results showed that the mean dry deposition velocities Of SO2 were 0.61 cm s(-1) during daytime and 0.27 cm s(-1) during nighttime. From the comparison of the monthly data, a tendency was observed that the dry deposition velocity increases with LAI and solar radiation. Furthermore, it was observed that the deposition velocity was larger over wet canopy than over dry canopy, and that higher deposition velocities in the wet season were mainly caused by non-stomatal uptake of wet canopy. Over wet canopy, the mean dry deposition velocities Of SO2 were estimated to be 0.83 cm s(-1) during daytime and 0.47 cm s(-1) during nighttime; and 0.44 cm s(-1) during daytime and 0.19 cm s(-1) during nighttime over dry canopy. There is good agreement between the results of this study and those in other studies and the predictions of Zhang et al. (2003a). The medians (geometric means) of derived r(c) during daytime are 233 (266) m s(-1) over dry canopy and 147 (146) m s(-1) over wet canopy. It was found that solar radiation is the critical important meteorological variable determining stomatal resistance during daytime. For non-stomatal resistance, clear dependencies were observed on the friction velocity and relative humidity. (C) 2009 Elsevier Ltd. All rights reserved.en_US
dc.language.isoen_USzh_TW
dc.relationAtmospheric Environmenten_US
dc.relation.ispartofseriesAtmospheric Environment, Volume 44, Issue 8, Page(s) 1011-1019.en_US
dc.relation.urihttp://dx.doi.org/10.1016/j.atmosenv.2009.12.022en_US
dc.subjectEast Asiaen_US
dc.subjectSulfur dioxideen_US
dc.subjectDry depositionen_US
dc.subjectStomatal and non-stomatalen_US
dc.subjectresistancesen_US
dc.subjectEvergreen broadleaf foresten_US
dc.subjectsulfur-dioxideen_US
dc.subjectnorthern thailanden_US
dc.subjectdeciduous foresten_US
dc.subjecttropical foresten_US
dc.subjectcloud foresten_US
dc.subjectozoneen_US
dc.subjectmodelen_US
dc.subjectparameterizationen_US
dc.subjectseasonen_US
dc.subjectatmosphereen_US
dc.titleObservation of SO2 dry deposition velocity at a high elevation flux tower over an evergreen broadleaf forest in Central Taiwanen_US
dc.typeJournal Articlezh_TW
dc.identifier.doi10.1016/j.atmosenv.2009.12.022zh_TW
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