Experimental confirmation of the turbulent origin of sporadic-E irregularities at midlatitudes

Details Experimental confirmation of the turbulent origin of sporadic-E irregularities at midlatitudes Experimental confirmation of the turbulent origin of sporadic-E irregularities at midlatitudes

Jun 1987

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1987ge%26ae..27..497k&link_type=abstract

Geomagnetizm i Aeronomiia (ISSN 0016-7940), vol. 27, May-June 1987, p. 497, 498. In Russian.

Physics

Atmospheric Turbulence, Ionospheric Disturbances, Midlatitude Atmosphere, Sporadic E Layer, Daytime, Inhomogeneity, Night Sky

Scientific paper

Ashkhabad data on the semitransparent sporadic-E layer are used to
determine a value of 4-5 for the p parameter, which corresponds to the
theoretical value of the index of the three-dimensional spectrum of
atmospheric turbulence. This confirms the turbulent nature of sporadic-E
irregularities pariticpating in the formation of radio reflections.

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