Summary
The results of comparisons of experimental data on the A3 2775 kHz absorption, X-ray (1–8 Å) flux and Lyman-α radiation are compared with model data on ionization-rate and radio-wave absorption height profiles. The Lyman-α radiation is found to dominate even in the upper D-region ionization (except flare conditions). A significant increase of usually used nitric oxide concentrations from rocket airglow measurements is required for achieving the best agreement between experimental and model data.
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References
C. A. Barth (1966a),Rocket measurement of the nitric oxide in the Upper Atmosphere, Planet. Space Sci.14, 623–630.
C. A. Barth (1966b),Nitric Oxide in the upper atmosphere, Ann. Géophys.22, 198–207.
G. Brasseur andM. Nicolet (1973),Chemospheric processes of nitric oxide in the mesosphere and stratosphere, Planet. Space Sci.21, 939–961.
CIRA 1972, COSPAR International Reference Atmosphere (Akademie-Verlag, Berlin 1972).
J. L. Culhane, P. W. Sanford, M. L. Shaw, K. J. H. Phillips, A. P. Willmore, P. J. Bowen, K. A. Pounds andD. C. Smith (1969),A study of the solar soft X-ray spectrum, Month. Not. R. Astr. Soc.145, 435–455.
D. G. Deeks (1966),Generalized full wave theory for energy-dependent collision frequencies, J. Atmos. Terr. Phys.28, 839–846.
K. P. Dere, D. M. Horan andR. W. Kreplin (1974),The spectral dependence of solar soft X-ray flux values obtained by SOLRAD 9, J. Atmos. Terr. Phys.36, 989–994.
J. E. Hall (1972),Atmospheric pressure, density and scale height calculated from H Lyman-β absorption allowing for the variation in cross-section with wavelength, J. Atmos. Terr. Phys.34, 1337–1348.
A. Haug andB. Landmark (1970),A two-ion model of electron-ion recombination in the D-region, J. Atmos. Terr. Phys.32, 405–407.
R. E. Huffman, D. E. Paulsen, J. R. Larrabee, andR. B. Cairns (1971),Decrease in D-region O2(1Δg)photoionization rates resulting from CO 2 absorption, J. Geophys. Res.76, 1028–1038.
R. M. Jones (1970),Ray theory for lossy media, Radio Sci.5, 793–801.
J. Laštovička (1973a),On the solar Lyman-α control of the ionospheric absorption at 2775 kHz, J. Atmos. Terr. Phys.35, 815–820.
J. Laštovička (1973b),Denní ionizace horní D-vrstvy zemské ionosféry, CSc. Thesis, Geophys. Inst., Prague (in Czech).
J. Laštovička (1974),On the role of the solar Lyman-α radiation in ionospheric absorption at 2775 kHz, Pure appl. Geophys.112, 655–663.
J. Laštovička (1975),Calculation of the upper D-region ionization by various ionization sources, Travaux Géophys. 1973, 431–446, Academia, Prague.
J. Laštovička (1976a),On the linearity of the dependence of the A3 ionospheric absorption at 2775 kHz on the intensity of ionizing radiation, J. Atmos. Terr. Phys.37, 1505–1510.
J. Laštovička (1976b),On some sources of uncertainty in Lyman-α ionization-rate calculation, Studia geoph. et geod.20 (in print).
J. Laštovička andP. Klas (1974),Calculation of the absorption height profile for the 2775 kHz Kiel-Panská Ves circuit, Travaux Géophys. 1974, Academia, Prague (in print).
J. Laštovička andP. Tříska (1974),Solar Lyman alpha control of the A3 ionospheric absorption on 2775 kHz, inMethods of Measurements and Results of Lower Ionosphere Structure (Akademie-Verlag, Berlin), 323–327.
K. Maeda (1969),Mid-latitude electron density profile as revealed by rocket experiments, J. Geomagn. Geoelectr.21, 557–567.
E. A. Mechtly andL. G. Smith (1970),Changes of lower ionosphere electron densities with solar zenith angle, Radio Sci.5, 1407–1412.
L. G. Meira (1971),Rocket measurements of upper atmospheric nitric oxide and their consequences to the lower ionosphere, J. Geophys. Res.76, 202–212.
B. A. Pontano andL. C. Hale (1970),Measurements of N ionizable constituents of the Low Ionosphere using a Lyman-α Source and Blunt Probe, Space Res. X, 208–214, North Holland, Amsterdam.
W. Singer andJ. Bremmer (1972),Mean electron density profiles of the D-region and their dependence on the solar zenith angle, Geomagn. Aeronom.12, 54–59 (in Russian).
L. G. Smith andK. L. Miller (1974),The measurement of O 2 number density by absorption of Lyman-α, J. Geophys. Res.79, 1965–1971.
W. Swider (1969),Ionization rates due to the attenuation of 1–100 Å nonflare solar X-rays in the terrestrial atmosphere, Rev. Geophys.7, 573–594.
E. V. Thrane andW. R. Piggott (1966),The collision frequency in the D- and E-regions of the ionosphere, J. Atmos. Terr. Phys.28, 721–737.
G. C. Tisone (1973),Measurements of NO densities during sunrise at Kauai, J. Geophys. Res.78, 746–750.
P. Tříska andJ. Laštovička (1970),On the X-ray control of the ionospheric absorption of HF radio waves, Solar Phys.15, 503–506.
P. Velinov (1968),On ionization in the ionospheric D-region by galactic and solar cosmic rays, J. Atmos. Terr. Phys.30, 1891–1905.
M. N. Vlasov (1975),Metastable particles and relation between charged and neutral components in the mesosphere, presented at Int. Symp. “Mesospheric and Ionospheric Structure Parameter Interaction,” Tallinn, USSR.
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Laštovička, J. The dependence of the ionospheric absorption at 2775 kHz on the intensity of ionizing radiation—Ionospheric implications. PAGEOPH 114, 321–331 (1976). https://doi.org/10.1007/BF00876933
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DOI: https://doi.org/10.1007/BF00876933