Sporadic E movement followed with a pencil beam high frequency radar

Details Sporadic E movement followed with a pencil beam high frequency radar Sporadic E movement followed with a pencil beam high frequency radar

Dec 1983

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1983p%26ss...31.1397f&link_type=abstract

Planetary and Space Science (ISSN 0032-0633), vol. 31, Dec. 1983, p. 1397-1407. Research supported by the Australian Research Gr

Computer Science

Sound

15

Cloud Physics, Ionospheric Sounding, Pencil Beams, Radar Measurement, Sporadic E Layer, High Frequencies, Shapes, Size (Dimensions)

Scientific paper

Several types of sporadic E are observed using the 5.80 and 3.84-MHz Bribie Island pencil-beam high-frequency radar. Blanketing Es takes the form of large flat sheets with ripples in them. Non-blanketing Es is observed to be small clouds that drift across the field of view (40 deg). There is continuous gradation of sporadic E structure between these extremes. There are at least four different physical means by which sporadic E clouds may apparently move. It is concluded that non-blanketing sporadic E consists of separate clouds which follow the movement of the constructive interference between internal gravity waves rather than being blown by the background wind.

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