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

Journal Article · · Journal of Geophysical Research: Atmospheres
DOI:https://doi.org/10.1029/2022jd038238· OSTI ID:1990138
 [1];  [2];  [1];  [3];  [4];  [5];  [6];  [7];  [8];  [9];  [9];  [10];  [1];  [11]
  1. Institute of Earth Physics and Space Science (EPSS) (Hungary)
  2. Institute of Earth Physics and Space Science (EPSS) (Hungary); Univ. of Szeged (Hungary)
  3. Massachusetts Inst. of Technology (MIT), Cambridge, MA (United States)
  4. Los Alamos National Laboratory (LANL), Los Alamos, NM (United States)
  5. CAESAR Consultancy, Cambridge (United Kingdom)
  6. Institute of Earth Physics and Space Science (EPSS) (Hungary); Eötvös Loránd University, Budapest (Hungary)
  7. University of Évora (Portugal)
  8. Polish Academy of Sciences (PAS), Warsaw (Poland)
  9. Vaisala, Louisville, CO (United States)
  10. Eötvös Loránd University, Budapest (Hungary); ELKH‐ELTE Space Research Group, Budapest (Hungary)
  11. HeartMath Institute, Boulder Creek, CA (United States)

Responses 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.

Research Organization:
Los Alamos National Laboratory (LANL), Los Alamos, NM (United States)
Sponsoring Organization:
USDOE Laboratory Directed Research and Development (LDRD) Program
Grant/Contract Number:
89233218CNA000001
OSTI ID:
1990138
Report Number(s):
LA-UR-23-23259
Journal Information:
Journal of Geophysical Research: Atmospheres, Journal Name: Journal of Geophysical Research: Atmospheres Journal Issue: 8 Vol. 128; ISSN 2169-897X
Publisher:
American Geophysical UnionCopyright Statement
Country of Publication:
United States
Language:
English

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