Neutral Winds, the Cause of Some Irregularities on the Sporadic E Layer

Details Neutral Winds, the Cause of Some Irregularities on the Sporadic E Layer Neutral Winds, the Cause of Some Irregularities on the Sporadic E Layer

Dec 2011

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011agufmsa31b1964n&link_type=abstract

American Geophysical Union, Fall Meeting 2011, abstract #SA31B-1964

Physics

[2439] Ionosphere / Ionospheric Irregularities, [2443] Ionosphere / Midlatitude Ionosphere

Scientific paper

An analytical analysis of the stratified shear flow theory under the conditions of the midlatitude Es is presented. Description of the analytical solution and its dependence of the winds and neutral density scale height is shown, as well as the predictions of the morphology for the irregularities according to the measured neutral winds for the E layer over Arecibo. We conclude that characteristics of the neutral winds and the properties of the neutral density profile are the clue to understanding the properties of the irregularities of the sporadic E layer. Examples of variability of this irregularities under different conditions is shown in the Figure 1.

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