O(1S) and O(1D) quantum yields from rocket measurements of electron densities and 557.7 and 630.0 nm emissions in the nocturnal F-region

[1]  M. Abdu,et al.  Solar activity effects on equatorial plasma bubble zonal velocity and its latitude gradient as measured by airglow scanning photometers , 1991 .

[2]  C. Tepley,et al.  Airglow intensities observed in the southern and northern hemispheres , 1990 .

[3]  D. R. Bates Oxygen green and red line emission and O2+ dissociative recombination , 1990 .

[4]  M. Abdu,et al.  Latitudinal gradient in the plasma bubble zonal velocities as observed by scanning 630-nm airglow measurements , 1990 .

[5]  S. Guberman,et al.  Collisional quenching of O(1D) by O(3P) , 1990 .

[6]  Y. Sahai,et al.  Equatorial f-region oi 6300 å and oi 5577 å emission profiles observed by rocket-borne airglow photometers , 1990 .

[7]  I. J. Kantor,et al.  Rocket-borne measurements of equatorial ionospheric electron densities and their comparison with IRI-10 predictions , 1990 .

[8]  Paul B. Hays,et al.  The auroral 6300 Å emission: Observations and modeling , 1988 .

[9]  L. Cogger,et al.  A reexamination of the O I 6300-Å nightglow , 1988 .

[10]  I. Batista,et al.  On the rocket-induced wave disturbances in the daytime equatorial ionosphere , 1988 .

[11]  J. Yee Non-thermal distribution of O(1D) atoms in the night-time thermosphere , 1988 .

[12]  H. Takahashi,et al.  Multispectral optical observations of ionospheric F-region storm effects at low latitude , 1987 .

[13]  S. Guberman The production of O(1S) from dissociative recombination of O2 + , 1987, Nature.

[14]  A. Hedin MSIS‐86 Thermospheric Model , 1987 .

[15]  S. Guberman The production of O(1D) from dissociative recombination of O2 , 1987 .

[16]  T. Killeen,et al.  Thermospheric production of O(1S) by dissociative recombination of vibrationally excited O2 , 1986 .

[17]  S. Solomon,et al.  The quenching rate of O(1D) by O(3P). [with data from Visible Airglow experiment on AE satellites , 1986 .

[18]  M. A. Abdu,et al.  Equatorial F region vertical plasma drifts: Seasonal and longitudinal asymmetries in the American sector , 1986 .

[19]  Y. Sahai,et al.  Equatorial plasma bubble eastward velocity characteristics from scanning airglow photometer measurements over cachoeira paulista , 1984 .

[20]  T. Killeen,et al.  O(¹S) from dissociative recombination of O2 +: Nonthermal line profile measurements from Dynamics Explorer , 1983 .

[21]  J. McConnell,et al.  An analysis of the spatial distribution of dayside cleft optical emissions , 1983 .

[22]  S. Solomon,et al.  The dissociative recombination of O2 +: The quantum yield of O(¹S) and O(¹D) , 1983 .

[23]  H. Takahashi,et al.  Simultaneous observations of OI 7774‐Å and [OI] 6300‐Å emissions and correlative study with ionospheric parameters , 1981 .

[24]  C. J. Zamlutti,et al.  Wave disturbances in the low latitude ionosphere and equatorial ionospheric plasma depletions , 1981 .

[25]  C. J. Zamlutti,et al.  Association between plasma bubble irregularities and airglow disturbances over Brazilian low latitudes , 1980 .

[26]  D. R. Bates,et al.  The O(1S) quantum yield from O2+ dissociative recombination , 1980 .

[27]  E. J. Weber,et al.  Airborne studies of equatorial F layer ionospheric irregularities , 1980 .

[28]  E. C. Zipf A laboratory study on the dissociative recombination of vibrationally excited O2 + ions , 1980 .

[29]  J. Meriwether,et al.  6300-Å airglow meridional intensity gradients , 1980 .

[30]  H. Takahashi,et al.  Plasma irregularities in the tropical F‐region detected by OI 7774 Å and 6300 Å nightglow measurements , 1980 .

[31]  J. Meriwether,et al.  F region airglow: Are ground-based observations consistent with recent satellite results? , 1980 .

[32]  E. C. Zipf The OI(¹S) state: Its quenching by O2 and formation by the dissociative recombination of vibrationally excited O2 + ions , 1979 .

[33]  D. R. Bates Forbidden oxygen and nitrogen lines in the nightglow , 1978 .

[34]  José Humberto,et al.  Optical measurements of the quenching coefficient of the O(1D) state by collisions with ambient molecules utilizing the ionospheric heating experiment , 1978 .

[35]  D. T. Farley,et al.  Nighttime dynamics of the F region near Arecibo as mapped by airglow features , 1978 .

[36]  J. Frederick,et al.  Morning and evening behavior of the F region green line emission: Evidence concerning the sources of O(¹S) , 1977 .

[37]  J. Meriwether,et al.  Contamination of ground-based measurements of OI (6300 Å) and NI (5200 Å) airglow by OH emissions , 1977 .

[38]  L. Jacchia,et al.  Thermospheric temperature, density, and composition: New models , 1977 .

[39]  J. Frederick,et al.  The O I (λ5577 Å) airglow: Observations and excitation mechanisms , 1976 .

[40]  H. Carlson,et al.  Combined airglow and incoherent scatter observations as a technique for studying neutral atmospheric variations , 1974 .

[41]  P. Hays,et al.  Twilight airglow: 1. Photoelectrons and [O I] 5577-Angstrom radiation , 1973 .

[42]  G. Hernandez The signature profiles of O(1S) In the airglow , 1971 .

[43]  R. Hake,et al.  Optical (λ6300) detection of radio frequency heating of electrons in the F region , 1970 .

[44]  V. L. Peterson Discussion of rocket nightglow data of I. S. Gulledge, D. M. Packer, S. G. Tilford, and J. T. Vanderslice , 1970 .

[45]  J. A. Greenspan Synoptic description of the 6300 Å nightglow near 78° west longitude , 1966 .

[46]  T. VanZandt,et al.  F-region nightglow emissions of atomic oxygen: 1. Theory , 1966 .