Votes and proceedings of the General Assembly of the state of New-Jersey . F-5 VERTICALPROFILES OFUNPERTURBED NITRICACID(HN03)AND NITROGENDIOXIDE (N02)AT MIDDLE LATITUDESObservations com-pared with calculatedfall-season valuesfromWldhopfs2Dzonallymodel. NOg Concentration, mo»ecu»es/cm F4 ZONAL (LONGITUDINAL) AVERAGES OF OZONE-COLUMN THICKNESS In Dobson units, vs. latitude during the fall season. Observationscompared with Widhopfs 20 The mld-latltude peek Isthought to result from poleward transport of ozone formed near theequator. § 500 - »f>V^ GeMwrt it a -Oct. F-7 STRATOSPHERIC VE
Votes and proceedings of the General Assembly of the state of New-Jersey . F-5 VERTICALPROFILES OFUNPERTURBED NITRICACID(HN03)AND NITROGENDIOXIDE (N02)AT MIDDLE LATITUDESObservations com-pared with calculatedfall-season valuesfromWldhopfs2Dzonallymodel. NOg Concentration, mo»ecu»es/cm F4 ZONAL (LONGITUDINAL) AVERAGES OF OZONE-COLUMN THICKNESS In Dobson units, vs. latitude during the fall season. Observationscompared with Widhopfs 20 The mld-latltude peek Isthought to result from poleward transport of ozone formed near theequator. § 500 - »f>V^ GeMwrt it a -Oct. F-7 STRATOSPHERIC VERTICAL TEMPERATUREPROFILE Computed by Callls et al uslna a thermally In-teractive photochemical The calculationIncludes the effect of Raylelgh scattering onphotolysis rates. U S Standard AttnCoupled ModelFull Sun45°, EquinoxNo Injection
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Keywords: ., bookauthornewjerseylegislaturegeneralassembly, bookidproceed00n
