Votes and proceedings of the General Assembly of the state of New-Jersey . ons or speciescan easily be left out. This has hap-pened frequently in aeronomy. sincenew processes are constantly beingdiscovered. F-3 displays vertical profiles ofcertain stratospheric constituentsclassed as important during the a fraction of these have beenmeasured Others, par-ticularly reactive radicals, have been inferred from model calculations. All the CIAP models included at•east the Chapman system involving O,O2 and O3, the NOx catalytic cycleinvolving NO and NO2. and some HOxradicals deri
Votes and proceedings of the General Assembly of the state of New-Jersey . ons or speciescan easily be left out. This has hap-pened frequently in aeronomy. sincenew processes are constantly beingdiscovered. F-3 displays vertical profiles ofcertain stratospheric constituentsclassed as important during the a fraction of these have beenmeasured Others, par-ticularly reactive radicals, have been inferred from model calculations. All the CIAP models included at•east the Chapman system involving O,O2 and O3, the NOx catalytic cycleinvolving NO and NO2. and some HOxradicals derived from water vapor ( etc). The more photochemicallycomplex models included photolysisand reformation of nitric acid (HNO3)and other nitrogen species, such as N,N2O. NO3. N2O5. and NH3; reactionsinvolving excited and ground states ofatomic and molecular oxygen OfD),0(3P), O^A) and O^J). and re-actions involving methane. CH4, andorganic methane derivatives (CH3,CH3O. CH3OO, CH3OH, HCO, etc.) Our own one-dimensional modelincluded over 100 reactions among CRS-285. F-4 VERTICAL PROFILESOF UNPERTURBED OZONE (O3JAND NITRIC OXIDE (NO)AT MIDDLE LATITUDES Observations compared withcalculated fall-season values fromWldhopfs 2D zonally averaged model. 3 4 5(i0)12Oj Conotnt ration, moitcul**/ m3 —I AcKtrmon tt 01 (1973)[44«N,A,Moy] O Ridtoyctgl (1974)[33*N, NovJU50%) D Sovo^t, «t 01 (1974) E
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