Release of NO(x) from sunlight-irradiated midlatitude snow
Document Type
Article
Publication Date
8-1-2000
Abstract
Photochemical production and release of gas-phase NO(x) (NO + NO < inf> 2 ) from the natural snowpack at a remote site in northern Michigan were investigated during the Snow Nitrogen and Oxidants in Winter study in January 1999. Snow was collected in an open 34 L chamber, which was then sealed with a transparent Teflon cover and used as an outdoor flow and reaction chamber. Significant increases in NO(x) mixing ratio were observed in synthetic and ambient air pulled through the sunlit chamber. [NO(x)] enhancements were correlated to ultraviolet sunlight intensity, reaching ~300 pptv under partially overcast midday, mid-winter conditions. These findings are consistent with NO(x) production from photolysis of snowpack NO < inf> 3 < sup> - ; the observed NO(x) release implies production of significant amounts of OH within the snow. Snowpack NO < inf> 3 < sup> - photolysis may therefore significantly alter boundary layer levels of both NO(x) and oxidized compounds over wide regions of the atmosphere.
Publication Title
Geophysical Research Letters
Recommended Citation
Honrath, R.,
Peterson, M.,
Dziobak, M.,
Dibb, J.,
Arsenault, M.,
&
Green, S.
(2000).
Release of NO(x) from sunlight-irradiated midlatitude snow.
Geophysical Research Letters,
27(15), 2237-2240.
http://doi.org/10.1029/1999GL011286
Retrieved from: https://digitalcommons.mtu.edu/michigantech-p/8268