Intense Equatorial Electrojet and Counter Electrojet Caused by the 15 January 2022 Tonga Volcanic Eruption: Space‐ and Ground‐Based Observations
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[1] K. Mandli,et al. Under the Surface: Pressure-Induced Planetary-Scale Waves, Volcanic Lightning, and Gaseous Clouds Caused by the Submarine Eruption of Hunga Tonga-Hunga Ha’apai Volcano Provide an Excellent Research Opportunity , 2022, Earthquake Research Advances.
[2] A. Coster,et al. 2022 Tonga Volcanic Eruption Induced Global Propagation of Ionospheric Disturbances via Lamb Waves , 2022, Frontiers in Astronomy and Space Sciences.
[3] D. Themens,et al. Global Propagation of Ionospheric Disturbances Associated With the 2022 Tonga Volcanic Eruption , 2022, Geophysical Research Letters.
[4] C. Englert,et al. Evaluation of Atmospheric 3‐Day Waves as a Source of Day‐to‐Day Variation of the Ionospheric Longitudinal Structure , 2021, Geophysical research letters.
[5] C. Stolle,et al. Neutral Wind Profiles During Periods of Eastward and Westward Equatorial Electrojet , 2021, Geophysical Research Letters.
[6] P. Alken,et al. Short‐Term Variability of Equatorial Electrojet Modulation by Solar Tidal and Planetary Waves, as Derived From the Swarm Constellation , 2021, Journal of Geophysical Research: Space Physics.
[7] C. Englert,et al. Validation of ICON‐MIGHTI Thermospheric Wind Observations: 2. Green‐Line Comparisons to Specular Meteor Radars , 2021, Journal of geophysical research. Space physics.
[8] C. Englert,et al. Validation of ICON‐MIGHTI Thermospheric Wind Observations: 1. Nighttime Red‐Line Ground‐Based Fabry‐Perot Interferometers , 2021, Journal of geophysical research. Space physics.
[9] R. Heelis,et al. Challenges to Understanding the Earth's Ionosphere and Thermosphere , 2020, Journal of Geophysical Research: Space Physics.
[10] M. E. Hagan,et al. Oscillation of the Ionosphere at Planetary‐Wave Periods , 2018, Journal of Geophysical Research: Space Physics.
[11] K. Groves,et al. Longitudinal and Seasonal Variability of Equatorial Ionospheric Irregularities and Electrodynamics , 2018, Space Weather.
[12] T. J. Immel,et al. The Ionospheric Connection Explorer Mission: Mission Goals and Design , 2018, Space science reviews.
[13] Scott Ellis,et al. Michelson Interferometer for Global High-Resolution Thermospheric Imaging (MIGHTI): Instrument Design and Calibration , 2017, Space Science Reviews.
[14] S. Wing,et al. Filamentary field-aligned currents at the polar cap region during northward interplanetary magnetic field derived with the Swarm constellation , 2016, Annales geophysicae.
[15] Irina Zakharenkova,et al. Prompt penetration electric fields and the extreme topside ionospheric response to the June 22–23, 2015 geomagnetic storm as seen by the Swarm constellation , 2016, Earth, Planets and Space.
[16] E. Yizengaw,et al. Response of the equatorial ionosphere to the geomagnetic DP 2 current system , 2016 .
[17] H. Lühr,et al. Magnetopause erosion during the 17 March 2015 magnetic storm: Combined field‐aligned currents, auroral oval, and magnetopause observations , 2016 .
[18] A. Chulliat,et al. Swarm equatorial electric field chain: First results , 2015 .
[19] F. Sassi,et al. On the day‐to‐day variation of the equatorial electrojet during quiet periods , 2014 .
[20] B. Damtie,et al. The longitudinal variability of equatorial electrojet and vertical drift velocity in the African and American sectors , 2014 .
[21] T. Pant,et al. Equatorial ionosphere-thermosphere system during geomagnetic storms , 2013 .
[22] S. Nayar,et al. Extreme changes in the equatorial electrojet under the influence of interplanetary electric field and the associated modification in the low‐latitude F region plasma distribution , 2012 .
[23] C. Denardini,et al. Climatology of gravity waves-induced electric fields in the equatorial E region , 2009 .
[24] F. Toffoletto,et al. How the Earth's inner magnetosphere works: An evolving picture , 2007 .
[25] G. Hulot,et al. Swarm: A constellation to study the Earth’s magnetic field , 2006 .
[26] David N. Anderson,et al. Daytime vertical E × B drift velocities inferred from ground‐based magnetometer observations at low latitudes , 2004 .
[27] R. Heelis,et al. Electrodynamics in the low and middle latitude ionosphere: a tutorial , 2004 .
[28] Jeffrey M. Forbes,et al. Migrating and nonmigrating diurnal tides in the middle and upper atmosphere excited by tropospheric latent heat release , 2002 .
[29] Timothy Fuller-Rowell,et al. Storm-time changes in the upper atmosphere at low latitudes , 2002 .
[30] H. Lühr,et al. Penetration of auroral electric fields to the equator during a substorm , 2000 .
[31] L. Scherliess,et al. Storm time dependence of equatorial disturbance dynamo zonal electric fields , 1997 .
[32] David L. Hysell,et al. JULIA radar studies of electric fields in the equatorial electrojet , 1997 .
[33] D. T. Farley,et al. Equatorial disturbance dynamo electric fields , 1983 .
[34] D. T. Farley,et al. Equatorial electric fields during magnetically disturbed conditions 1. The effect of the interplanetary magnetic field , 1979 .
[35] B. Fejer,et al. An explanation for anomalous equatorial ionospheric electric fields associated with a northward turning of the interplanetary magnetic field , 1979 .
[36] A. Richmond,et al. Thermospheric response to a magnetic substorm , 1975 .
[37] A. Richmond. Equatorial electrojet-I. Development of a model including winds and instabilities , 1973 .
[38] S. Maus,et al. Noon‐time equatorial electrojet: Its spatial features as determined by the CHAMP satellite , 2004 .
[39] D. Cunnold. The equatorial electrojet. , 1978 .