The equatorial E-region and its plasma instabilities: a tutorial

DT Farley - Annales Geophysicae, 2009 - angeo.copernicus.org
In this short tutorial we first briefly review the basic physics of the E-region of the equatorial
ionosphere, with emphasis on the strong electrojet current system that drives plasma …

Effects of electrojet turbulence on a magnetosphere‐ionosphere simulation of a geomagnetic storm

M Wiltberger, V Merkin, B Zhang… - Journal of …, 2017 - Wiley Online Library
Ionospheric conductance plays an important role in regulating the response of the
magnetosphere‐ionosphere system to solar wind driving. Typically, models of …

Kinetic simulations of 3‐D Farley‐Buneman turbulence and anomalous electron heating

MM Oppenheim, YS Dimant - Journal of Geophysical Research …, 2013 - Wiley Online Library
Electric fields map from the magnetosphere to the E region ionosphere where they drive the
intense currents of the auroral electrojet. Particularly during geomagnetic storms and …

Joule heating in the thermosphere

AD Richmond - Upper atmosphere dynamics and energetics, 2021 - Wiley Online Library
High‐latitude Joule heating is an important energy source for thermospheric dynamics and
composition. It is influenced by winds, plasma turbulence, variable electric fields, and …

Point-cloud clustering and tracking algorithm for radar interferometry

MF Ivarsen, JP St-Maurice, GC Hussey… - Physical Review E, 2024 - APS
In data mining, density-based clustering, which entails classifying datapoints according to
their distributions in some space, is an essential method to extract information from large …

Deriving the ionospheric electric field from the bulk motion of radar aurora in the E‐region

MF Ivarsen, JP St‐Maurice… - Journal of …, 2024 - Wiley Online Library
In the auroral E‐region strong electric fields can create an environment characterized by fast
plasma drifts. These fields lead to strong Hall currents which trigger small‐scale plasma …

Magnetosphere‐ionosphere coupling through E region turbulence: 2. Anomalous conductivities and frictional heating

YS Dimant, MM Oppenheim - Journal of Geophysical Research …, 2011 - Wiley Online Library
Global magnetospheric MHD codes using ionospheric conductances based on laminar
models systematically overestimate the cross–polar cap potential during storm time by up to …

Narrow width Farley‐Buneman spectra above 100 km altitude

JP St‐Maurice, D Huyghebaert… - Journal of …, 2023 - Wiley Online Library
For spectra associated with full turbulence the observed mean phase velocity of unstable
Farley‐Buneman waves has been found not to exceed the ion‐acoustic speed, cs. This has …

Photoelectron‐induced waves: A likely source of 150 km radar echoes and enhanced electron modes

MM Oppenheim, YS Dimant - Geophysical Research Letters, 2016 - Wiley Online Library
VHF radars near the geomagnetic equator receive coherent reflections from plasma density
irregularities between 130 and 160 km in altitude during the daytime. Though researchers …

First 3‐D simulations of meteor plasma dynamics and turbulence

MM Oppenheim, YS Dimant - Geophysical Research Letters, 2015 - Wiley Online Library
Millions of small but detectable meteors hit the Earth's atmosphere every second, creating
trails of hot plasma that turbulently diffuse into the background atmosphere. For over 60 …