Generation of ELF waves during HF heating of the ionosphere at midlatitudes

A. S. Sharma, B. Eliasson, X. Shao, K. Papadopoulos

Research output: Contribution to journalArticle

4 Citations (Scopus)

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.
LanguageEnglish
Pages962-971
Number of pages10
JournalRadio Science
Volume51
Issue number7
Early online date14 Jul 2016
DOIs
Publication statusPublished - 14 Jul 2016

Fingerprint

Ionosphere
temperate regions
ionospheres
ionosphere
magnetohydrodynamic waves
heating
Heating
F region
magnetospheres
ionospherics
cyclotrons
Magnetosphere
radio frequency heating
Cyclotrons
electromagnetism
Plasmas
plasma
Hall currents
ions
magnetosphere

Keywords

  • mid-latitude ionosphere
  • ELF waves
  • ionospheric heating

Cite this

Sharma, A. S. ; Eliasson, B. ; Shao, X. ; Papadopoulos, K. / Generation of ELF waves during HF heating of the ionosphere at midlatitudes. In: Radio Science. 2016 ; Vol. 51, No. 7. pp. 962-971.
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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 Alfv{\'e}n 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.",
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Generation of ELF waves during HF heating of the ionosphere at midlatitudes. / Sharma, A. S.; Eliasson, B.; Shao, X.; Papadopoulos, K.

In: Radio Science, Vol. 51, No. 7, 14.07.2016, p. 962-971.

Research output: Contribution to journalArticle

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AU - Sharma, A. S.

AU - Eliasson, B.

AU - Shao, X.

AU - Papadopoulos, K.

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AB - 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.

KW - mid-latitude ionosphere

KW - ELF waves

KW - ionospheric heating

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