2010
DOI: 10.1016/j.atmosenv.2009.12.022
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Observation of SO2 dry deposition velocity at a high elevation flux tower over an evergreen broadleaf forest in Central Taiwan

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Cited by 18 publications
(14 citation statements)
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“…The V d of O 3 and SO 2 lie well within the range of values determined for other tropical forests (Matsuda et al, 2006, Rummel et al, 2007Tsai et al, 2010) and grasslands (Takahashi et al, 2001;Sorimachi et al, 2003). The modeled V d of NO 2 and NH 3 are within a reasonable range compared to reference values (Zhang et al, 2005Trebs et al, 2006;Kirkman et al, 2002;Delon et al, 2010;Endo et al, 2011).…”
Section: Dry Deposition Velocitiessupporting
confidence: 59%
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“…The V d of O 3 and SO 2 lie well within the range of values determined for other tropical forests (Matsuda et al, 2006, Rummel et al, 2007Tsai et al, 2010) and grasslands (Takahashi et al, 2001;Sorimachi et al, 2003). The modeled V d of NO 2 and NH 3 are within a reasonable range compared to reference values (Zhang et al, 2005Trebs et al, 2006;Kirkman et al, 2002;Delon et al, 2010;Endo et al, 2011).…”
Section: Dry Deposition Velocitiessupporting
confidence: 59%
“…In fact, there exists a marked latitudinal gradient over the west and central African zone. Areas with the highest rainfall have the greatest volume of biomass or primary productivity; as a consequence, surface deposition (cuticle) and stomatal uptake become important, and the canopy resistance (R c ) is the main factor determining the deposition rate in vegetative zones (Tsai et al, 2010).…”
Section: Dry Deposition Velocitiesmentioning
confidence: 99%
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