Winds in the 70-200 km height range
General discussion of upper atmosphere winds in 70 to 200 kilometer range
WIND↗
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Preliminary results of measurements of the height of ionosphere inhomogeneities by signals from artificial earth satellites <predvaritel'nyye rezul'taty izmereniy vysoty ionosfernykh neodnorodnostey po signalam isz<
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Yerukhimov, L. M.↗
On the analysis and interpretation of winds observed at heights of 85 to 135 kilometers - A rebuttal.
Winds in upper atmosphere as revealed by sodium vapor trails explained on basis of prevailing and tidal components critically analyzed
UPPER ATMOSPHERE↗
Earth as an occulting disk for study of solar EUV emission heights.
Source distributions of UV and X-ray emission in corona and chromosphere determined from flight of spacecraft-borne instruments into Earth shadow
OCCULTATION↗
Spectrometric investigation of the ozone layer to the height of 60 km spektrometricheskoye issledovaniye ozonnogo sloya do vysoty 60 km
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Britayev, A. S.↗
Effective absorption height of radio waves in the cm band in the oxygen atmosphere and in water vapor ob effektivnoy vysote pogloshcheniya radiovoln santimetrovogo diapazona v atmosfernom kislorode i vodyanom pare
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Kuzovlev, V. V.↗
Investigation of cosmic radiation at heights of 200-350 km on the satellites cosmos 4 and cosmos 7 issledovaniye kosmicheskogo izlucheniya na vysotakh 200-350 km na sputnikakh kosmos-4 i kosmos-7
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Basilova, R. N.↗
Solid-state time-to-pulse-height converter developed
Solid-state circuit produces an output pulse with an amplitude directly proportional to the time interval between two input pulses. It uses selected circuit options to achieve variable mode operation and a tunnel diode controls the charging time of a capacitor in proportion to the time interval being measured.
Lynch, R. J.↗
Turbulent motions in the upper atmosphere at heights of 80-110 km according to radio observations of meteor trains
Turbulence in upper atmosphere according to radio echo observations of meteor trains
METEOR TRAIL↗
Notes on thunderstorm motions, heights, and circulations
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WEATHER FORECASTING↗
Atmospheric tides in the height region 90 to 120 kilometers.
E region atmospheric tides from chemical release trails observations, obtaining prevailing diurnal and semidiurnal components
Justus, C. G.↗
Pulse-height analyzer with digital readout
Feedback-controlled pulse-amplitude integrator and amplifier is used as an analog-to-digital converter that converts event-liberated charges, emanating from a nuclear-particle detector, directly to numbers rather than to analog-dependent voltages.
Goldsworthy, W. W.↗
Suggested test of a self-calibrating baro- height reporting concept for general aviation and airline SSR Interim scientific report
Self-calibrating baro-altitude concept for general aviation
Source record↗
Morphology of electron concentration enhancement at a height of 1000 kilometers at polar latitudes.
Electron concentration enhancement in upper atmosphere at polar latitudes, noting three independent zones and relation to magnetic local time
Colin, L.↗
Wide-range pulse-height discriminator
Improved pulse amplitude discriminator has discriminator level in millivolt range, permits simple adjustment over wide range, and is stable within one percent at temperatures between minus 20 degrees and plus 60 degrees C. The discriminator responds to narrow pulses /500 nsec/, draws little power /milliwatts/, and requires simple circuitry.
Cancro, C. A.↗
On-line data analysis of digital pulse-height spectra. Part 1 - Analytical structure. Part 2 - Operational computer systems
On-line digital analysis of geochemical spectra data
Schmadeback, R. L.↗
Potential time-cost benefits from use of orbital-height photographic data in cartographic programs
Cost effectiveness of mapping using satellite- borne photography
Sibert, W.↗
Correlation of radar backscattering cross sections with ocean wave height and wind velocity
Ocean surface condition correlation to radar backscattering cross sections and wind velocity from scatterometer data
Krishen, K.↗