Generation of ELF waves during HF heating of the ionosphere at midlatitudes
Sharma, A. S. and Eliasson, B. and Shao, X. and Papadopoulos, K. (2016) Generation of ELF waves during HF heating of the ionosphere at midlatitudes. Radio Science, 51 (7). pp. 962-971. ISSN 0048-6604 (https://doi.org/10.1002/2016RS005953)
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Abstract
Modulated high frequency radio frequency heating of the ionospheric F-region produces a local modulation of the electron temperature, and the resulting pressure gradient gives rise to a diamagnetic current. The oscillations of the diamagnetic current excite hydromagnetic waves in the ELF range that propagate away from the heated region. The generation of the waves in the 2 - 10 Hz range by a modulated heating in the midlatitude ionosphere is studied using numerical simulations of a collisional Hall-magnetohydrodynamic model. To model the plasma processes in the midlatitude ionosphere the Earth's dipole magnetic field and typical ionospheric plasma parameters are used. As the hydromagnetic waves propagate away from the heated region in the F-region, the varying plasma conditions lead to changes in their characteristics. Magnetosonic waves generated in the heating region and propagating down to the E-region, where the Hall conductivity is dominant, excite oscillating Hall currents that produce shear Alfvén waves propagating along the field lines into the magnetosphere, where they propagate as the electromagnetic ion cyclotron (EMIC) and whistler waves. The EMIC waves propagate to the ion cyclotron resonance layer in the magnetosphere, where they are absorbed.
ORCID iDs
Sharma, A. S., Eliasson, B. ORCID: https://orcid.org/0000-0001-6039-1574, Shao, X. and Papadopoulos, K.;-
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Item type: Article ID code: 56166 Dates: DateEvent14 July 2016Published14 July 2016Published Online13 April 2016AcceptedSubjects: Science > Physics Department: Faculty of Science > Physics Depositing user: Pure Administrator Date deposited: 15 Apr 2016 08:55 Last modified: 15 Nov 2024 01:08 Related URLs: URI: https://strathprints.strath.ac.uk/id/eprint/56166