The Extreme Solar and Geomagnetic Storms on 20-25 March 1940

Author:

Hayakawa Hisashi1234ORCID,Oliveira Denny M56,Shea Margaret A7,Smart Don F7,Blake Seán P58,Hattori Kentaro9ORCID,Bhaskar Ankush T10,Curto Juan J11,Franco Daniel R12,Ebihara Yusuke13

Affiliation:

1. Institute for Space-Earth Environmental Research, Nagoya University, Nagoya, 4648601, Japan

2. Institute for Advanced Research, Nagoya University, Nagoya, 4648601, Japan

3. UK Solar System Data Centre, Space Physics and Operations Division, RAL Space, Science and Technology Facilities Council, Rutherford Appleton Laboratory, Harwell Oxford, Didcot, Oxfordshire, OX11 0QX, UK

4. Nishina Centre, Riken, Wako, 3510198, Japan

5. Heliophysics Science Division, NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA

6. Goddard Planetary Heliophysics Institute, University of Maryland, Baltimore County, Baltimore, MD, United States

7. SSSRC, 100 Tennyson Avenue, Nashua, NH 03062, USA

8. Catholic University of America, Washington DC, United States

9. Graduate School of Science, Kyoto University, Kyoto, 6068501, Japan

10. Space Physics Laboratory, Vikram Sarabhai Space Centre, ISRO, Thiruvananthapuram, 695022, Kerala, India

11. Observatori de l'Ebre, (OE) CSIC – URL, 43520, Roquetes, Spain

12. Department of Geophysics, National Observatory of Brazil, São Cristóvão, 20921-400, RJ, Brazil

13. Research Institute for Sustainable Humanosphere, Kyoto University, Uji, 6110011, Japan

Abstract

Abstract In late March 1940, at least five significant solar flares were reported. They likely launched interplanetary coronal mass ejections (ICMEs), and were associated with one of the largest storm sudden commencements (SSCs) since the year 1868, resulting in space weather hazards that today would have significant societal impacts. The initial solar activity is associated with a short geomagnetic storm and a notable SSC. Afterward, the third flare was reported in the eastern solar quadrant (N12 E37-38) at 11:30–12:30 UT on 23 March, with significant magnetic crochets (up to ≈ |80| nT at Eskdalemuir) during 11:07–11:40 UT. On their basis, we estimate the required energy flux of the source flare as X35±1 in soft X-ray class. The resultant ICMEs caused enormous SSCs (up to > 425 nT recorded at Tucson) and allowed us to estimate an extremely inward magnetopause position (estimated magnetopause standoff position ≈ 3.4 RE). The time series of the resultant geomagnetic storm is reconstructed using a Dst estimate, which peaked at 20 UT on 24 March at ≈ −389 nT. Around the storm main phase, the equatorial boundary of the auroral oval extended ≤ 46.3° at invariant latitudes. This sequence also caused a solar proton event and Forbush decrease (≈ 3%). These sequences indicate pileups of multiple ICMEs, which even achieved a record value of inward magnetopause position. Our analyses of this historical pioneer event bring more insights into possible serious space weather hazards and provide a quantitative basis for future analyses and predictions.

Publisher

Oxford University Press (OUP)

Subject

Space and Planetary Science,Astronomy and Astrophysics

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