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Multi-instrument detection in Europe of ionospheric disturbances caused by the 15 January 2022 eruption of the Hunga volcano
  • +12
  • Tobias Verhulst,
  • David Altadill,
  • Veronika Barta,
  • Anna Belehaki,
  • Dalia Buresova,
  • Claudio Cesaroni,
  • Ivan Galkin,
  • Marco Guerra,
  • Alessandro Ippolito,
  • Themistocles Herekakis,
  • Daniel Kouba,
  • Antoni Segarra,
  • Luca Spogli,
  • Ioanna Tsagouri,
  • Jens Mielich
Tobias Verhulst
Royal Meteorological Institute of Belgium, Royal Meteorological Institute of Belgium, Royal Meteorological Institute of Belgium

Corresponding Author:[email protected]

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David Altadill
Observatori de l’Ebre, CSIC – Universitat Ramon Llull, Roquetes, Spain, Observatori de l’Ebre, CSIC – Universitat Ramon Llull, Roquetes, Spain, Observatori de l’Ebre, CSIC – Universitat Ramon Llull, Roquetes, Spain
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Veronika Barta
Institute of Earth Physics and Space Science, Sopron, Hungary, Institute of Earth Physics and Space Science, Sopron, Hungary, Institute of Earth Physics and Space Science, Sopron, Hungary
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Anna Belehaki
National Observatory of Athens, National Observatory of Athens, National Observatory of Athens
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Dalia Buresova
Institute of Atmospheric Physics of the Czech Academy of Sciences, Institute of Atmospheric Physics of the Czech Academy of Sciences, Institute of Atmospheric Physics of the Czech Academy of Sciences
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Claudio Cesaroni
Istituto Nazionale di Geofisica e Vulcanologia, Rome, Italy, Istituto Nazionale di Geofisica e Vulcanologia, Rome, Italy, Istituto Nazionale di Geofisica e Vulcanologia, Rome, Italy
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Ivan Galkin
University of Massachusetts Lowell, University of Massachusetts Lowell, University of Massachusetts Lowell
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Marco Guerra
SpacEarth Technology, Rome, Italy, SpacEarth Technology, Rome, Italy, SpacEarth Technology, Rome, Italy
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Alessandro Ippolito
Istituto Nazionale di Geofisica e Vulcanologia, Rome, Italy, Istituto Nazionale di Geofisica e Vulcanologia, Rome, Italy, Istituto Nazionale di Geofisica e Vulcanologia, Rome, Italy
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Themistocles Herekakis
National Observatory of Athens, National Observatory of Athens, National Observatory of Athens
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Daniel Kouba
Institute of Atmospheric Physics of the Czech Academy of Sciences, Institute of Atmospheric Physics of the Czech Academy of Sciences, Institute of Atmospheric Physics of the Czech Academy of Sciences
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Antoni Segarra
Observatori del Ebre, Observatori del Ebre, Observatori del Ebre
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Luca Spogli
Istituto Nazionale di Geofisica e Vulcanologia, Istituto Nazionale di Geofisica e Vulcanologia, Istituto Nazionale di Geofisica e Vulcanologia
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Ioanna Tsagouri
National Observatory of Athens, National Observatory of Athens, National Observatory of Athens
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Jens Mielich
Leibniz-Institute of Atmospheric Physics, Kühlungsborn, Germany, Leibniz-Institute of Atmospheric Physics, Kühlungsborn, Germany
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Abstract

The 15 January 2022 eruption of the Hunga volcano provides a unique opportunity to study the reaction of the ionosphere to large explosive events. In particular, this event allows us to study the global propagation of travelling ionospheric disturbances using various instruments. We focus on the detection of the ionospheric disturbances caused by this eruption over Europe, where dense networks of both ionosondes and GNSS receivers are available. This event took place on the day of a geomagnetic storm. We show how data from different instruments and from different observatories can be combined to clearly distinguish the TIDs produced by the eruption from those caused by concurrent geomagnetic activity. By comparing observations obtained from multiple types of instruments, we also show that TIDs produced by various mechanisms are present simultaneously, with different types of waves affecting different physical quantities.