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Dynamics of density cavities generated by frictional heating: Formation, distortion, and instability
Author(s) -
Zettergren M. D.,
Semeter J. L.,
Dahlgren H.
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 - 10.1002/2015gl066806
Subject(s) - instability , geophysics , convection , mesoscale meteorology , ionosphere , electric field , polar , physics , plasma , f region , earth's magnetic field , distortion (music) , density gradient , mechanics , computational physics , magnetic field , geology , meteorology , amplifier , quantum mechanics , astronomy , optoelectronics , cmos
Abstract A simulation study of the generation and evolution of mesoscale density cavities in the polar ionosphere is conducted using a time‐dependent, nonlinear, quasi‐electrostatic model. The model demonstrates that density cavities, generated by frictional heating, can form in as little as 90 s due to strong electric fields of ∼120 mV/m, which are sometimes observed near auroral zone and polar cap arcs. Asymmetric density cavity features and strong plasma density gradients perpendicular to the geomagnetic field are naturally generated as a consequence of the strong convection and finite extent of the auroral feature. The walls of the auroral density cavities are shown to be susceptible to large‐scale distortion and gradient‐drift instability, hence indicating that arc‐related regions of frictional heating may be a source of polar ionospheric density irregularities.