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Wind/WAVES observations of auroral kilometric radiation:: automated burst detection and terrestrial solar wind ‐ magnetosphere coupling effects

Wind/WAVES observations of auroral kilometric radiation:: automated burst detection and terrestrial solar wind ‐ magnetosphere coupling effects
Wind/WAVES observations of auroral kilometric radiation:: automated burst detection and terrestrial solar wind ‐ magnetosphere coupling effects
Auroral Kilometric Radiation (AKR) is the strongest terrestrial radio emission, and emanates from the same electron acceleration regions from which particles precipitate into the ionosphere, exciting the aurorae and other phenomena. As such, AKR is a barometer for the state of solar wind - magnetosphere - ionosphere coupling. AKR is anisotropically beamed in a hollow cone from a source region generally found at nightside local times, meaning that a single source region cannot be viewed from all local times in the magnetosphere. In radio data such as dynamic spectra, AKR is frequently observed simultaneously to other radio emissions which can have a similar intensity and frequency range, making it difficult to automatically detect. Building on a previously published pipeline to extract AKR emissions from Wind/WAVES data, in this paper a novel automated AKR burst detection technique is presented and applied to Wind/WAVES data. Over a five year interval, about 5000 AKR bursts are detected with median burst length ranging from about 30 to 60 min. During detected burst windows, higher solar wind velocity is observed, and the interplanetary magnetic field clock angle is observed to tend toward BZ < 0, BY < 0, when compared with the entire statistical interval. Additionally, higher geomagnetic activity is observed during burst windows at polar, high and equatorial latitudes.
2169-9380
Fogg, A.R.
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Jackman, C.M.
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Waters, J.E.
7e6a7887-ad91-4b04-963e-48c734e778ed
Bonnin, X.
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Lamy, L.
aad11182-ba51-4937-99f3-cf983891abdd
Cecconi, B.
eade7145-f6d1-4a0c-ad3d-9defe711c9d0
Issautier, K.
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Louis, C. K.
e11408ed-3b79-4d6c-98b0-654b91a91c74
Fogg, A.R.
c0610d4b-e88c-4598-b6fb-a9c1fb8db0be
Jackman, C.M.
9bc3456c-b254-48f1-ade0-912c5b8b4529
Waters, J.E.
7e6a7887-ad91-4b04-963e-48c734e778ed
Bonnin, X.
19da5602-2dac-4fad-a0fe-bde2683fda37
Lamy, L.
aad11182-ba51-4937-99f3-cf983891abdd
Cecconi, B.
eade7145-f6d1-4a0c-ad3d-9defe711c9d0
Issautier, K.
9354fb42-cb07-4125-90a4-01c4cc20da5c
Louis, C. K.
e11408ed-3b79-4d6c-98b0-654b91a91c74

Fogg, A.R., Jackman, C.M., Waters, J.E., Bonnin, X., Lamy, L., Cecconi, B., Issautier, K. and Louis, C. K. (2022) Wind/WAVES observations of auroral kilometric radiation:: automated burst detection and terrestrial solar wind ‐ magnetosphere coupling effects. Journal of Geophysical Research: Space Physics, 127 (5), [e2021JA030209]. (doi:10.1029/2021JA030209).

Record type: Article

Abstract

Auroral Kilometric Radiation (AKR) is the strongest terrestrial radio emission, and emanates from the same electron acceleration regions from which particles precipitate into the ionosphere, exciting the aurorae and other phenomena. As such, AKR is a barometer for the state of solar wind - magnetosphere - ionosphere coupling. AKR is anisotropically beamed in a hollow cone from a source region generally found at nightside local times, meaning that a single source region cannot be viewed from all local times in the magnetosphere. In radio data such as dynamic spectra, AKR is frequently observed simultaneously to other radio emissions which can have a similar intensity and frequency range, making it difficult to automatically detect. Building on a previously published pipeline to extract AKR emissions from Wind/WAVES data, in this paper a novel automated AKR burst detection technique is presented and applied to Wind/WAVES data. Over a five year interval, about 5000 AKR bursts are detected with median burst length ranging from about 30 to 60 min. During detected burst windows, higher solar wind velocity is observed, and the interplanetary magnetic field clock angle is observed to tend toward BZ < 0, BY < 0, when compared with the entire statistical interval. Additionally, higher geomagnetic activity is observed during burst windows at polar, high and equatorial latitudes.

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More information

e-pub ahead of print date: 13 April 2022
Published date: 1 May 2022

Identifiers

Local EPrints ID: 477944
URI: http://eprints.soton.ac.uk/id/eprint/477944
ISSN: 2169-9380
PURE UUID: a6234423-11f4-45c2-93c1-e89efbd09500
ORCID for A.R. Fogg: ORCID iD orcid.org/0000-0003-1213-4324
ORCID for C.M. Jackman: ORCID iD orcid.org/0000-0003-0635-7361
ORCID for J.E. Waters: ORCID iD orcid.org/0000-0001-8164-5414

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Date deposited: 16 Jun 2023 16:51
Last modified: 17 Mar 2024 01:39

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Contributors

Author: A.R. Fogg ORCID iD
Author: C.M. Jackman ORCID iD
Author: J.E. Waters ORCID iD
Author: X. Bonnin
Author: L. Lamy
Author: B. Cecconi
Author: K. Issautier
Author: C. K. Louis

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