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Hosokawa K, Kataoka R, Tsuda TT, Ogawa Y, Taguchi S, Zhang Y, Paxton LJ. Exceptionally gigantic aurora in the polar cap on a day when the solar wind almost disappeared. SCIENCE ADVANCES 2024; 10:eadn5276. [PMID: 38905334 PMCID: PMC11192072 DOI: 10.1126/sciadv.adn5276] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 12/14/2023] [Accepted: 05/15/2024] [Indexed: 06/23/2024]
Abstract
Revealing the origins of aurorae in Earth's polar cap has long been a challenge since direct precipitation of energetic electrons from the magnetosphere is not always expected in this region of open magnetic field lines. Here, we introduce an exceptionally gigantic aurora filling the entire polar cap region on a day when the solar wind had almost disappeared. By combining ground-based and satellite observations, we proved that this unique aurora was produced by suprathermal electrons streaming directly from the Sun, which is known as "polar rain." High-sensitivity imaging from the ground has visualized complex spatial structures of the polar rain aurora possibly manifesting the internal pattern of the solar wind or even the organizations in the chromosphere of the Sun.
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Affiliation(s)
- Keisuke Hosokawa
- Graduate School of Communication Engineering and Informatics, University of Electro-Communications, Tokyo 182-8585, Japan
- Center for Space Science and Radio Engineering, University of Electro-Communications, Tokyo 182-8585, Japan
| | - Ryuho Kataoka
- National Institute of Polar Research, Tokyo 190-0014, Japan
| | - Takuo T. Tsuda
- Graduate School of Communication Engineering and Informatics, University of Electro-Communications, Tokyo 182-8585, Japan
- Center for Space Science and Radio Engineering, University of Electro-Communications, Tokyo 182-8585, Japan
| | - Yasunobu Ogawa
- National Institute of Polar Research, Tokyo 190-0014, Japan
| | - Satoshi Taguchi
- Graduate School of Science, Kyoto University, Kyoto 606-8502, Japan
| | - Yongliang Zhang
- The Johns Hopkins University Applied Physics Laboratory, Laurel, MD 20723, USA
| | - Larry J. Paxton
- The Johns Hopkins University Applied Physics Laboratory, Laurel, MD 20723, USA
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Wilcox JM, Duffy PB, Schatten KH, Svalgaard L, Scherrer PH, Roberts WO, Olson RH. Interplanetary Magnetic Field Polarity and the Size of Low-Pressure Troughs Near 180{degrees}W Longitude. Science 1979; 204:60-2. [PMID: 17816739 DOI: 10.1126/science.204.4388.60] [Citation(s) in RCA: 21] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/02/2022]
Abstract
When the interplanetary magnetic field is directed away from the sun, the area of wintertime low-pressure (300-millibar) troughs near 180 degrees W longitude is significantly larger than when the field is toward the sun. This relation persists during most of the winters of 1951 to 1973.
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