Votes and proceedings of the General Assembly of the state of New-Jersey . 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. CRS-287 F-8 AN OVERVIEW OF OZONE-REDUCTION ESTIMATES Summary of CIAP calculations of percent total ozone reduction from a uniformlydistributed stratospheric NOx source at 20 km. The circled 1 data pointsidentify Johnstons original photochemical equilibrium (
Votes and proceedings of the General Assembly of the state of New-Jersey . 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. CRS-287 F-8 AN OVERVIEW OF OZONE-REDUCTION ESTIMATES Summary of CIAP calculations of percent total ozone reduction from a uniformlydistributed stratospheric NOx source at 20 km. The circled 1 data pointsidentify Johnstons original photochemical equilibrium (OD) calculations. Theother models assume 1D vertical transport except for the 2D (vertical andlatitudinal) transport models of Hesstvedt. Vupputun. Widhopf and Brasseur andBerlin and the 3D (MIT) model of Cunnold et al Numbers in parentheses denotereference numbers in this A IA articlelOOrr
Size: 1573px × 1589px
Photo credit: © The Reading Room / Alamy / Afripics
License: Licensed
Model Released: No
Keywords: ., bookauthornewjerseylegislaturegeneralassembly, bookidproceed00n
