Responses of the AC/DC Global Electric Circuit to Volcanic Electrical Activity in the Hunga Tonga‐Hunga Ha'apai Eruption on 15 January 2022

Author:

Bór J.1ORCID,Bozóki T.12ORCID,Sátori G.1ORCID,Williams E.3,Behnke S. A.4ORCID,Rycroft M. J.5ORCID,Buzás A.16,Silva H. G.7ORCID,Kubicki M.8ORCID,Said R.9ORCID,Vagasky C.9ORCID,Steinbach P.1011ORCID,André K. Szabóné1ORCID,Atkinson M.12

Affiliation:

1. Institute of Earth Physics and Space Science (EPSS) Sopron Hungary

2. Department of Optics and Quantum Electronics University of Szeged Szeged Hungary

3. Parsons Laboratory of the Department of Civil and Environmental Engineering Massachusetts Institute of Technology Cambridge MA USA

4. Space and Remote Sensing Los Alamos National Laboratory Los Alamos NM USA

5. CAESAR Consultancy Cambridge UK

6. Doctoral School of Earth Sciences Faculty of Science Eötvös Loránd University Budapest Hungary

7. Department of Physics University of Évora Évora Portugal

8. Institute of Geophysics Polish Academy of Sciences Warsaw Poland

9. Vaisala Louisville CO USA

10. Department of Geophysics and Space Science Eötvös Loránd University Budapest Hungary

11. ELKH‐ELTE Space Research Group Budapest Hungary

12. HeartMath Institute Boulder Creek CA USA

Abstract

AbstractResponses of the AC and DC global electric circuits (GECs) to the large eruption of the Hunga Tonga‐Hunga Ha'apai (HT‐HH) volcano on 15 January 2022 are discussed. The AC‐related investigation is based on Schumann resonance (SR) measurements from six stations on four continents. The DC‐related investigation utilizes atmospheric electric field (potential gradient, PG) measurements from six recording stations in Europe and the USA. According to data from the GLD360 and WWLLN lightning detection networks, the peak lightning stroke rate, 83/s, was dominated by negative polarity lightning, but the distributions of positive and negative lightning discharges in latitude and longitude around the volcano differed. A global intensification of SR is apparent in connection with the enhanced lightning activity caused by the eruption. SR data‐based results confirm that the lightning activity in the eruption dominated the naturally occurring global activity for a period of about 1 hr. The highly localized increase in lightning activity over HT‐HH was a unique point source of SR excitation. PG measurements suggest that impulse‐like charging of the DC GEC, by ∼15%, via negative cloud‐to‐ground lightning strokes took place twice during the eruption. A time constant of 7 or 8 min has been inferred for near‐surface PG changes due to these enhancements. This could be the first direct measurement of the time constant of the GEC near the Earth's surface, as well as the first observation of the direct charging of the DC GEC by a unique atmospheric electrified source.

Funder

National Research, Development and Innovation Office

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Geophysics

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