posted on 2018-08-15, 10:57authored byAngeline G. Burrell, Gareth W. Perry, Timothy K. Yeoman, Stephen E. Milan Milan, Russell Stoneback
Coherent‐scatter, high‐frequency, phased‐array radars create narrow beams through the use of constructive and destructive interference patterns. This formation method leads to the creation of a secondary beam, or lobe, that is sent out behind the radar. This study investigates the relative importance of the beams in front of and behind the high‐frequency radar located in Hankasalmi, Finland, using observations taken over a solar cycle, as well as coincident observations from Hankasalmi and the Enhanced Polar Outflow Probe Radio Receiver Instrument. These observations show that the relative strength of the front and rear beams is frequency dependent, with the relative amount of power sent to the front lobe increasing with increasing frequency. At the range of frequencies used by Hankasalmi, both front and rear beams are always present, though the main beam is always stronger than the rear lobe. Because signals are always transmitted to the front and rear of the radar, it is always possible to receive backscatter from both return directions. Examining the return direction as a function of local time, season, and solar cycle shows that the dominant return direction depends primarily on the local ionospheric structure. Diurnal changes in plasma density typically cause an increase in the amount of groundscatter returning from the rear lobe at night, though the strength of this variation has a seasonal dependence. Solar cycle variations are also seen in the groundscatter return direction, modifying the existing local time and seasonal variations.
Funding
A. G. Burrell, S. E. Milan, and
T. K. Yeoman were supported by
NERC grant NE/K011766/1. The
research at the University of Calgary
was supported by the Natural
Sciences and Engineering Research
Council of Canada (NSERC) Discovery
Grant Program and Discovery
Accelerator Supplement Program.
The development and operations
of the CASSIOPE/e-POP mission
were supported by the Industrial
Technologies Office (ITO), Canadian
Space Agency (CSA), and MacDonald,
Dettwiler and Associates (MDA),
respectively. R. Stoneback was supported
by NSF grant 1259508.
e-POP RRI data can be accessed at
http://epop-data.phys.ucalgary.ca.
The authors acknowledge the use
of IDL GEOPACK DLM in the production
of the RRI data products used
in this work. The authors acknowledge
the use of SuperDARN data.
SuperDARN is a collection of radars
funded by the national scientific funding
agencies of Australia, Canada,
China, France, Italy, Japan, Norway,
South Africa, the United Kingdom,
and the United States. The Virginia
Tech SuperDARN database (described
at http://vt.superdarn.org/) provides
up-to-date public access to the
Hankasalmi observations, which were
analyzed with the aid of DaViTpy. We
acknowledge use of NASA/GSFC’s
Space Physics Data Facility’s OMNIWeb
service and OMNI data. Galactic
Cosmic Ray data were obtained from
the Sodankyla Geophysical Observatory
at http://cosmicrays.oulu.fi. GPS
TEC data products and access through
the Madrigal distributed data system
are provided to the community by the
Massachusetts Institute of Technology
under support from U.S. National Science
Foundation grant AGS-1242204.
Data for the TEC processing is provided
by the following organizations:
UNAVCO, Scripps Orbit and Permanent
Array Center, Institut Geographique
National, France, International GNSS
Service, The Crustal Dynamics Data
Information System (CDDIS), National
Geodetic Survey, Instituto Brasileiro
de Geografia e Estatística, RAMSAC
CORS of Instit
History
Citation
Radio Science, 2018, 53 (4), pp. 577-597 (21)
Author affiliation
/Organisation/COLLEGE OF SCIENCE AND ENGINEERING/Department of Physics and Astronomy
Version
VoR (Version of Record)
Published in
Radio Science
Publisher
American Geophysical Union (AGU),Wiley, International Union of Radio Science
The file associated with this record is under embargo until six months after publication, in accordance with the publisher's self-archiving policy. The full text may be available through the publisher links provided above.