Investigation of horizontal structures at mesospheric altitudes using coherent radar imaging

The Middle Atmosphere Alomar Radar System (MAARSY) in Northern Norway (69.30°N, 16.04°E) was used to perform interferometric observations of Polar Mesosperic Summer Echoes (PMSE) in June 2012. Coherent Radar Imaging (CRI) using Capon's method was applied allowing a high spatial resolution. The...

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Bibliographic Details
Main Authors: Sommer, S., Stober, G., Schult, C., Zecha, M., Latteck, R.
Format: Article in Journal/Newspaper
Language:English
Published: Göttingen : Copernicus 2013
Subjects:
ddc:550
Beam pattern
Coherent radar
Head echoes
High spatial resolution
Middle atmosphere
Scattering centers
Scattering width
Short periods
Algorithms
Radar imaging
Radar systems
Scattering
Holography
Northern Norway
Online Access:https://oa.tib.eu/renate/handle/123456789/5591
https://doi.org/10.34657/4220
Description
Summary:The Middle Atmosphere Alomar Radar System (MAARSY) in Northern Norway (69.30°N, 16.04°E) was used to perform interferometric observations of Polar Mesosperic Summer Echoes (PMSE) in June 2012. Coherent Radar Imaging (CRI) using Capon's method was applied allowing a high spatial resolution. The algorithm was validated by simulation and trajectories of meteor head echoes. Both data sets show a good correspondence with the algorithm. Using this algorithm, the aspect sensitivity of PMSE was analysed in a case study, making use of the capability of CRI to resolve the pattern within the beam volume. No correction of the beam pattern was made yet. It was found in this case study, that no large variations in the scattering width and the scattering center occured apart from a very short period of time at the upper edge of the PMSE.

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