Premium
First artificial periodic inhomogeneity experiments at HAARP
Author(s) -
Hysell D. L.,
McCarrick M. J.,
Fallen C. T.,
Vierinen J.
Publication year - 2015
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1002/2015gl063064
Subject(s) - ionosonde , doppler effect , ambipolar diffusion , computational physics , physics , altitude (triangle) , diffusion , noise (video) , tokamak , antenna (radio) , plasma , ionosphere , optics , geophysics , electron density , nuclear physics , astronomy , computer science , telecommunications , geometry , mathematics , artificial intelligence , image (mathematics) , thermodynamics
Experiments involving the generation and detection of artificial periodic inhomogeneities have been performed at the High Frequency Active Auroral Research Program (HAARP) facility. Irregularities were created using powerful X ‐mode HF emissions and then probed using short (10 μs) X ‐ and O ‐mode pulses. Reception was performed using a portable software‐defined receiver together with the crossed rhombic antenna from the local ionosonde. Echoes were observed reliably between about 85 and 140 km altitude with signal‐to‐noise ratios as high as about 30 dB. The Doppler shift of the echoes can be associated with the vertical neutral wind in this altitude range. Small but persistent Doppler shifts were observed. The decay time constant of the echoes is meanwhile indicative of the ambipolar diffusion coefficient which depends on the plasma temperature, composition, and neutral gas density. The measured time constants appear to be consistent with theoretical expectations and imply a methodology for measuring neutral density profiles. The significance of thermospheric vertical neutral wind and density measurements which are difficult to obtain using ground‐based instruments by other means is discussed.