Halocarbon concentration patterns associated with frontal passages

The atmospheric mixing ratios of CCl2F2 (F-12) and CCl3F (F-11) increase abruptly up to 14 ppt (F-12) and 8 ppt (F-11) after strong cold fronts pass and decrease abruptly after warm fronts pass at a semicontinuous monitoring station near Pullman, WA (46 deg 42 min N, 117 deg 10 min W). It is conclud...

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Veröffentlicht in:	Geophys. Res. Lett.; (United States) 1983-11, Vol.10 (11), p.1100-1103
Hauptverfasser:	Carter, M. W., Cronn, D. R., Bamesberger, W. L., Robinson, E.
Format:	Artikel
Sprache:	eng
Schlagworte:	500200 - Environment, Atmospheric- Chemicals Monitoring & Transport- (-1989) AIR Air masses CHALCOGENIDES Chemical composition and interactions. Ionic interactions and processes Cold fronts DISASTERS EARTH ATMOSPHERE Earth, ocean, space Environment Pollution ENVIRONMENTAL SCIENCES ENVIRONMENTAL TRANSPORT Exact sciences and technology External geophysics FEDERAL REGION X FLUIDS FREONS GASES Geophysics HALOGENATED ALIPHATIC HYDROCARBONS Latitude MASS TRANSFER Meteorology Monitoring NITROGEN COMPOUNDS NITROGEN OXIDES NITROUS OXIDE Nitrous oxides NORTH AMERICA ORGANIC COMPOUNDS ORGANIC HALOGEN COMPOUNDS OXIDES OXYGEN COMPOUNDS Stations STORMS SURFACE AIR TROPOSPHERE USA Warm fronts WASHINGTON WIND
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