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au.\*:("NORTON RB")

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MOLECULAR OXYGEN BETWEEN 95 AND 210 KM DETERMINED FROM SOBRAD 10 OCCULTATION MEASUREMENTS.NORTON RB; ROBLE RG.1974; J. GEOPHYS. RES.; U.S.A.; DA. 1974; VOL. 79; NO 35; PP. 3876-3878; BIBL. 12 REF.Article

CHANGES IN THERMOSPHERIC COMPOSITION INFERRED FROM TWILIGHT O+(2P) EMISSIONNOXON JF; NORTON RB.1979; PLANET. SPACE SCI.; GBR; DA. 1979; VOL. 27; NO 5; PP. 653-663; BIBL. 21 REF.Article

THERMOSPHERIC MOLECULAR OXYGEN FROM SOLAR EXTREME-ULTRAVIOLET OCCULTATION MEASUREMENTSROBLE RG; NORTON RB.1972; J. GEOPHYS. RES.; U.S.A.; DA. 1972; VOL. 77; NO 19; PP. 3524-3533; BIBL. 1P.1/2Serial Issue

NO3 IN THE TROPOSPHERENOXON JF; NORTON RB; MAROVICH E et al.1980; GEOPHYS. RES. LETTERS; USA; DA. 1980; VOL. 7; NO 2; PP. 125-128; BIBL. 9 REF.Article

EFFECT OF A MAJOR WARMING UPON STRATOSPHERIC NO2NOXON JF; MAROVICH E; NORTON RB et al.1979; J. GEOPHYS. RES.; USA; DA. 1979; VOL. 84; NO C12; PP. 7883-7888; BIBL. 6 REF.Article

OBSERVATION OF ATMOSPHERIC NO3NOXON JF; NORTON RB; HENDERSON WR et al.1978; GEOPHYS. RES. LETTERS; USA; DA. 1978; VOL. 5; NO 8; PP. 675-678; BIBL. 10 REF.Article

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