Spatial correlation of auroral radio absorption /

The temporal behavior of auroral radio absorption measured with riometers at medium and high latitudes displays complex patterns that differ spatially. These differences may be limited to a time-displacement of otherwise similar absorption patterns, indicating a movement which could be interpreted i...

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Bibliographic Details
Main Authors: Toman, Kurt., Corbett, John J., Cormier, Raymond J., Air Force Cambridge Research Laboratories (U.S.)
Format: Text
Language:English
Published: L.G. Hanscom Field, Bedford, Massachusetts : Air Force Cambridge Research Laboratories, Air Force Systems Command, United States Air Force 1971
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Online Access:http://hdl.handle.net/2027/mdp.39015095137041
Description
Summary:The temporal behavior of auroral radio absorption measured with riometers at medium and high latitudes displays complex patterns that differ spatially. These differences may be limited to a time-displacement of otherwise similar absorption patterns, indicating a movement which could be interpreted in terms of a structured, locally enhanced, precipitating, energetic particle stream that moves over a geographic area while preserving its structure. In order to assess numerically the spatial coherence of auroral radio absorption, a correlation study of such absorption patterns has been undertaken. Data were recorded by more than eight riometer stations during five days of varying activity containing the magnetic storm of 18 April 1965. With a day as the sample size, the results of this study provide a view of the spatial coherence of auroral absorption which could be exploited further for the prediction of ionospheric propagation in the arctic. (Author). Presented at the AGARD-NATO Wave Propagation Panel Specialists Meeting on Radar Propagation in the Arctic, held at Max Planck Institute for Aeronomy, Lindau/Harz, 13 to 17 September 1971. AD 0739168 (from http://www.dtic.mil). N72-26140. "17 September 1971." Includes bibliographical references (page 13). The temporal behavior of auroral radio absorption measured with riometers at medium and high latitudes displays complex patterns that differ spatially. These differences may be limited to a time-displacement of otherwise similar absorption patterns, indicating a movement which could be interpreted in terms of a structured, locally enhanced, precipitating, energetic particle stream that moves over a geographic area while preserving its structure. In order to assess numerically the spatial coherence of auroral radio absorption, a correlation study of such absorption patterns has been undertaken. Data were recorded by more than eight riometer stations during five days of varying activity containing the magnetic storm of 18 April 1965. With a day as the sample size, the results of this study provide a view of the spatial coherence of auroral absorption which could be exploited further for the prediction of ionospheric propagation in the arctic. (Author). Mode of access: Internet.