FIELD: geophysics. SUBSTANCE: method refers to remote measurements of parameters of lower ionosphere. It consists in emission of probing pulse into ionosphere, in reception of signal scattered back by inhomogeneities of ionospheric plasma, in determination of amplitude dependence of signal scattered back and in determination of altitudes of turbulent layers by it. Preliminary action with powerful radio emission on frequency higher than critical for E layer and lower than critical for F layer of ionosphere is conducted. In consequence of it artificial periodic inhomogeneities having the least intensity at altitudes where intensive turbulent layers exist are emerging. EFFECT: enhanced authenticity and decreased time of measurements. 2 dwg
| Title | Year | Author | Number |
|---|---|---|---|
| METHOD FOR DETERMINING SPEED OF PLASMA TURBULENT MOVEMENT IN MESOSPHERE AND BOTTOM THERMOSPHERE | 2016 |
|
RU2638952C1 |
| METHOD FOR DETERMINING THE AMBIPOLAR DIFFUSION COEFFICIENT IN THE EARTH'S LOWER IONOSPHERE | 2018 |
|
RU2696015C1 |
| METHOD OF DETERMINING ELECTRON-ION RECOMBINATION TIME IN IONOSPHERE D-REGION | 0 |
|
SU1762290A1 |
| METHOD FOR DETERMINING THE TIGHTNESS OF ATMOSPHERE AT THE ALTITUDES OF E-IONOSPHERE | 0 |
|
SU1732309A1 |
| METHOD FOR DETERMINING THE ATOMIC MASS OF METAL IONS IN THE SPORADIC LAYER E (ES) | 2017 |
|
RU2660119C1 |
| METHOD TO DETERMINE THE TIGHTNESS OF ATMOSPHERE AT THE ALTITUDES OF E-IONOSPHERE | 0 |
|
SU1732310A1 |
| METHOD OF DETERMINING HIGH PROFILE OF ELECTRONIC CONCENTRATION IN ARTIFICIALLY DISTURBED LOWER IONOSPHERE | 0 |
|
SU1569758A1 |
| 0 |
|
SU1253308A1 | |
| METHOD OF CONTROLLING PROPAGATION OF SHORT RADIO WAVES IN IONOSPHERIC WAVEGUIDE | 2009 |
|
RU2413363C1 |
| METHOD OF CREATING RADIO CHANNEL THROUGH ARTIFICIAL IONOSPHERIC TRANSPONDER | 2012 |
|
RU2518900C2 |
