1978
DOI: 10.1016/0021-9169(78)90110-1
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Solar activity variation of nitric oxide in the E-region and its implications

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Cited by 16 publications
(3 citation statements)
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“…The discrepancies between the present model and the other two are due to the fact that both Chakrabarty et a1 (1978) and Roble et a1 (1978) suppose thermal equilibrium between electrons and neutrals when they calculate the recombination coefficient rates, while in situ measurements of T, show that this temperature is twice the neutral gas temperature at low solar activity. These two theoretical models differ in the n ( N 0 ) profiles used: while Roble eta/( 1978) solve a steady-state continuity equation for n(NO), Chakrabarty et al(1978) fit the n ( N 0 ) profile in order that the electron number density may agree with the observations. In the present model as discussed earlier, it is not necessary to propose an n ( N 0 ) profile since it is determined from the measured ne profile (see equation (10)).…”
Section: Application Of the Modelmentioning
confidence: 99%
“…The discrepancies between the present model and the other two are due to the fact that both Chakrabarty et a1 (1978) and Roble et a1 (1978) suppose thermal equilibrium between electrons and neutrals when they calculate the recombination coefficient rates, while in situ measurements of T, show that this temperature is twice the neutral gas temperature at low solar activity. These two theoretical models differ in the n ( N 0 ) profiles used: while Roble eta/( 1978) solve a steady-state continuity equation for n(NO), Chakrabarty et al(1978) fit the n ( N 0 ) profile in order that the electron number density may agree with the observations. In the present model as discussed earlier, it is not necessary to propose an n ( N 0 ) profile since it is determined from the measured ne profile (see equation (10)).…”
Section: Application Of the Modelmentioning
confidence: 99%
“…while Roble eta/( 1978) solve a steady-state continuity equation for n(NO), Chakrabarty et al(1978) fit the n ( N 0 ) profile in order that the electron number density may agree with the observations. In the present model as discussed earlier, it is not necessary to propose an n ( N 0 ) profile since it is determined from the measured ne profile (see equation ( 10)).…”
Section: Application Of the Modelmentioning
confidence: 99%
“…In order to investigate the solar variation of thermospheric NO, the observational data are not enough since the satellite observations were done only during a minimum phase of solar activity and rocket observations are sparse. However, the variability of a factor of 3 to 4 has been suggested from the change in the composition of the Eregion (CHAKRABARTY et al, 1978) as well as the gamma band airglow observation (OGAWA et al,1984). IWAGAMI and OGAWA (1987) Figure 1 represents the results of data discrimination between the gamma band and background emissions.…”
Section: Introductionmentioning
confidence: 99%