On the kinetic theory of subauroral arcs
E Mishin, A Streltsov - Journal of Geophysical Research: Space …, 2022 - Wiley Online Library
We report on a novel scenario of subauroral arcs within strong subauroral ion drifts (SAID)‐
STEVE and Picket Fence. Their explanation requires a local source of low‐energy, ε< 18.75 …
STEVE and Picket Fence. Their explanation requires a local source of low‐energy, ε< 18.75 …
Effects of electrojet turbulence on a magnetosphere‐ionosphere simulation of a geomagnetic storm
Ionospheric conductance plays an important role in regulating the response of the
magnetosphere‐ionosphere system to solar wind driving. Typically, models of …
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 …
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 …
composition. It is influenced by winds, plasma turbulence, variable electric fields, and …
The mysterious green streaks below STEVE
J Semeter, M Hunnekuhl, E MacDonald… - AGU …, 2020 - Wiley Online Library
Strong thermal emission velocity enhancement (STEVE) is an optical phenomenon of the
subauroral ionosphere arising from extreme ion drift speeds. STEVE consists of two distinct …
subauroral ionosphere arising from extreme ion drift speeds. STEVE consists of two distinct …
A time‐dependent two‐dimensional model simulation of lower ionospheric variations under intense SAID
J Liang, JP St‐Maurice… - Journal of Geophysical …, 2021 - Wiley Online Library
The subauroral ion drift (SAID) denotes a latitudinally narrow channel of fast westward ion
drift in the subauroral region, often observed during geomagnetically disturbed intervals …
drift in the subauroral region, often observed during geomagnetically disturbed intervals …
Model of anomalous electron heating in the E region: 1. Basic theory
Numerous radar observations demonstrate anomalously strong electron heating in polar
electrojets during magnetic storms. The effect often correlates with the onset of the Farley …
electrojets during magnetic storms. The effect often correlates with the onset of the Farley …
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 …
models systematically overestimate the cross–polar cap potential during storm time by up to …
Plasma wave heating during extreme electric fields in the high‐latitude E region
H Bahcivan - Geophysical Research Letters, 2007 - Wiley Online Library
This article presents measurements of electron heating in the high‐latitude E region during
rare, extreme convection electric fields (up to 160 mV/m). As inferred from the merged …
rare, extreme convection electric fields (up to 160 mV/m). As inferred from the merged …
A theoretical framework for the changing spectral properties of meter‐scale Farley‐Buneman waves between 90 and 125 km altitudes
JP St.‐Maurice, JL Chau - Journal of Geophysical Research …, 2016 - Wiley Online Library
Stimulated by recent observations described in a companion paper, we have revisited
existing theories of the Farley‐Buneman instability throughout the altitude range 90 to 125 …
existing theories of the Farley‐Buneman instability throughout the altitude range 90 to 125 …