Please use this identifier to cite or link to this item: http://hdl.handle.net/2248/8621
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dc.contributor.authorVichare, Geeta-
dc.contributor.authorBhaskar, Ankush-
dc.contributor.authorRawat, Rahul-
dc.contributor.authorYadav, Virendra-
dc.contributor.authorMishra, Wageesh-
dc.contributor.authorAngchuk, D-
dc.contributor.authorSingh, Anand Kumar-
dc.date.accessioned2024-12-18T08:35:56Z-
dc.date.available2024-12-18T08:35:56Z-
dc.date.issued2024-12-20-
dc.identifier.citationThe Astrophysical Journal, Vol. 977, No. 2, 171en_US
dc.identifier.issn1538-4357-
dc.identifier.urihttp://hdl.handle.net/2248/8621-
dc.descriptionOpen Accessen_US
dc.descriptionOriginal content from this work may be used under the terms of the Creative Commons Attribution 4.0 licence. Any further distribution of this work must maintain attribution to the author(s) and the title of the work, journal citation and DOI-
dc.description.abstractIn 2023 April, a low-latitude aurora observed by the all-sky camera at Hanle, Ladakh, India (33°14'N geographic latitude), generated significant interest. This was the first such aurora recorded from the Indian region in the space era and occurred during a moderate solar storm. This study explores this low-latitude auroral sighting, which happened during the sheath-region passage of an interplanetary coronal mass ejection. We analyze in situ multispacecraft particle measurements and geomagnetic field observations from both ground-based and satellite-based magnetometers. The auroral observations at Hanle coincided with intense substorm activity. Our findings indicate that the aurora did not actually reach India; the equatorward boundary was beyond 50°N geographic latitude. Enhanced electron fluxes with energies below 100 eV were detected at 54°N geographic latitude at about 830 km altitude in the predawn sector (4–5 hr local time). In the midnight sector, the equatorward boundary is estimated to be around 52°N geographic latitude, based on Hanle observations and considering emission altitudes of 600–650 km due to low-energy electrons. Thus, the low-latitude red aurora observed from India resulted from the emissions at higher altitudes due to low-energy electron precipitation in the auroral oval and a slight equatorward expansion of the auroral oval. The low-energy electrons likely originated from the plasma sheet and were precipitated due to enhanced wave–particle interactions from strong magnetosphere compression during high solar wind pressure. This study is crucial in understanding low-latitude auroras in the modern space era.en_US
dc.language.isoenen_US
dc.publisherAmerican Astronomical Societyen_US
dc.relation.urihttps://doi.org/10.3847/1538-4357/ad8dd3-
dc.rights© 2024. The Author(s)-
dc.subjectAuroraeen_US
dc.subjectSolar particle emissionen_US
dc.subjectSolar stormen_US
dc.subjectSolar coronal mass ejectionsen_US
dc.titleLow-latitude auroras: insights from 2023 april 23 solar stormen_US
dc.typeArticleen_US
Appears in Collections:IIAP Publications

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