2017
DOI: 10.1134/s1990793117060161
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Vertical Velocities and Temperature of the Neutral Component in the Upper Atmosphere

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Cited by 11 publications
(2 citation statements)
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“…The atmospheric temperature and density are determined from the API relaxation time, which is inversely proportional to the ambipolar diffusion coefficient. Many results of studying the altitude-temporal variations of temperature and density in different geo-and helio-physical conditions are presented in Reference [23][24][25][26][27][28].…”
Section: Experimental Backgroundmentioning
confidence: 99%
See 1 more Smart Citation
“…The atmospheric temperature and density are determined from the API relaxation time, which is inversely proportional to the ambipolar diffusion coefficient. Many results of studying the altitude-temporal variations of temperature and density in different geo-and helio-physical conditions are presented in Reference [23][24][25][26][27][28].…”
Section: Experimental Backgroundmentioning
confidence: 99%
“…Experimental data are presented in Table 1. Now, it is possible to apply out projection operators (26,27,28) and then to calculate, separately, energies for each mode, using formula (37), which need to be rewritten in the discrete form by replacement of integrals with sums, i.e., using midpoint rule. Since points are spaced, and we are interested in relative values only, simple sums can be used.…”
Section: Neutral Atmosphere Parameters Obtained Using Api Techniquementioning
confidence: 99%