NSEE Yielding Electron Temperature Measurements at the Arecibo Observatory. Issue 5 (21st May 2019)

• Record Type: Journal Article
• Authors: Mahmoudian, A.; Nossa, E.; Isham, B.; Bernhardt, P. A.; Briczinski, S. J.; Sulzer, M.
• Is Part Of: Journal of geophysical research. Volume 124:Issue 5(2019)
• Page Start: 3699
• Page End: 3708
• Publication Date: 2019-05-21
• Subjects: Magnetospheric physics -- Periodicals; Space environment -- Periodicals; Cosmic physics -- Periodicals; Planets -- Atmospheres -- Periodicals; Heliosphere (Astrophysics) -- Periodicals; Geophysics -- Periodicals; 523.01
• DOI: 10.1029/2019JA026594
• Languages: English
• ISSNs: 2169-9380

Abstract

Abstract: Narrowband stimulated electromagnetic emissions (NSEE), a component of radio emissions created during high‐frequency (HF) radiowave ionospheric modification experiments, occur within 1 kHz of the HF pump frequency. NSEE was observed and studied for the first time at the HAARP (High Frequency Active Auroral Research Program) facility in Alaska (Norin et al., 2009, https://doi.org/10.1103/PhysRevLett.102.065003 ; Bernhardt et al., 2010, https://doi.org/10.1103/PhysRevLett.104.165004 ). Magnetized stimulated Brillouin scatter (MSBS) is a component of NSEE, which was also first observed at HAARP (Norin et al., 2009, https://doi.org/10.1103/PhysRevLett.102.065003 ; Bernhardt et al., 2010, https://doi.org/10.1103/PhysRevLett.104.165004 ) and later at European Incoherent Scatter Scientific Association (Fu et al., 2015, https://doi.org/10.5194/angeo-33-983-2015 ). Ion‐acoustic and electrostatic ion cyclotron modes are the daughter products of MSBS and can be used for the determination of the electron temperature and of the presence of minor ion species, respectively, in the HF‐modified ionosphere. Here we present the first observations of the MSBS process at magnetic midlatitudes, excited during radio wave ionospheric modification experiments at the Arecibo Observatory. The NSEE observations, in combination with a theoretical model and the wave matching conditions, are used to estimate background ionospheric parameters. A qualitative comparison of the MSBS component of the NSEE spectrum with the thermal ion line measured by incoherent scatter radar is presented. Key Points: First NSEE observations at the Arecibo Observatory is reported Electron temperature estimation using NSEE spectral components is presented Reproduction of ISR observations using MSBS IA spectral line is discussed