Dayside magnetic ULF power at high latitudes: A possible long-term proxy for the solar wind velocity?

We examine the occurrence of dayside high-latitude magnetic variations with periods between 2 and 10 min statistically using data from around 20 magnetic stations in Greenland, Scandinavia, and Canada, many of which have been in operation for a full solar cycle. We derive time series of the power sp...

Full description

Bibliographic Details
Main Author: Vennerstrøm, Susanne
Format: Article in Journal/Newspaper
Language:English
Published: 1999
Subjects:
Online Access:https://orbit.dtu.dk/en/publications/6a9b2c47-68b8-47ba-b6e4-0aa385079fa7
id ftdtupubl:oai:pure.atira.dk:publications/6a9b2c47-68b8-47ba-b6e4-0aa385079fa7
record_format openpolar
spelling ftdtupubl:oai:pure.atira.dk:publications/6a9b2c47-68b8-47ba-b6e4-0aa385079fa7 2024-09-15T18:09:58+00:00 Dayside magnetic ULF power at high latitudes: A possible long-term proxy for the solar wind velocity? Vennerstrøm, Susanne 1999 https://orbit.dtu.dk/en/publications/6a9b2c47-68b8-47ba-b6e4-0aa385079fa7 eng eng https://orbit.dtu.dk/en/publications/6a9b2c47-68b8-47ba-b6e4-0aa385079fa7 info:eu-repo/semantics/restrictedAccess Vennerstrøm , S 1999 , ' Dayside magnetic ULF power at high latitudes: A possible long-term proxy for the solar wind velocity? ' , Journal of Geophysical Research-space Physics , vol. 104 , no. A5 , pp. 10145-10157 . article 1999 ftdtupubl 2024-06-25T14:25:27Z We examine the occurrence of dayside high-latitude magnetic variations with periods between 2 and 10 min statistically using data from around 20 magnetic stations in Greenland, Scandinavia, and Canada, many of which have been in operation for a full solar cycle. We derive time series of the power spectral density (psd) in two different frequency bands: 2-4 min period and 5-10 min period. The average psd in these bands maximizes in the early morning sector between auroral and cusp latitudes. The solar cycle variation of the average psd in the two bands during the morning hours is markedly different from the solar cycle variation of regular geomagnetic activity, measured by indices such as aa and Dst. The spectral band power is generally at minimum just prior to solar maximum and has a strong maximum in the late declining phase associated with high-speed streams from coronal holes. We have compared the spectral band power with satellite observations of the solar wind velocity and find a high log-linear correlation in the range 0.7-0.8. The highest correlation is found in the 2-4 min band. Contrary to this, the correlation with Bs and upsilon Bs is very weak (similar to 0.0-0.2), except in the 5-10 min band for the auroral stations. We find the results encouraging for the use of dayside spectral band power at high-latitude stations as a tool for investigating past solar wind variations. Article in Journal/Newspaper Greenland Technical University of Denmark: DTU Orbit
institution Open Polar
collection Technical University of Denmark: DTU Orbit
op_collection_id ftdtupubl
language English
description We examine the occurrence of dayside high-latitude magnetic variations with periods between 2 and 10 min statistically using data from around 20 magnetic stations in Greenland, Scandinavia, and Canada, many of which have been in operation for a full solar cycle. We derive time series of the power spectral density (psd) in two different frequency bands: 2-4 min period and 5-10 min period. The average psd in these bands maximizes in the early morning sector between auroral and cusp latitudes. The solar cycle variation of the average psd in the two bands during the morning hours is markedly different from the solar cycle variation of regular geomagnetic activity, measured by indices such as aa and Dst. The spectral band power is generally at minimum just prior to solar maximum and has a strong maximum in the late declining phase associated with high-speed streams from coronal holes. We have compared the spectral band power with satellite observations of the solar wind velocity and find a high log-linear correlation in the range 0.7-0.8. The highest correlation is found in the 2-4 min band. Contrary to this, the correlation with Bs and upsilon Bs is very weak (similar to 0.0-0.2), except in the 5-10 min band for the auroral stations. We find the results encouraging for the use of dayside spectral band power at high-latitude stations as a tool for investigating past solar wind variations.
format Article in Journal/Newspaper
author Vennerstrøm, Susanne
spellingShingle Vennerstrøm, Susanne
Dayside magnetic ULF power at high latitudes: A possible long-term proxy for the solar wind velocity?
author_facet Vennerstrøm, Susanne
author_sort Vennerstrøm, Susanne
title Dayside magnetic ULF power at high latitudes: A possible long-term proxy for the solar wind velocity?
title_short Dayside magnetic ULF power at high latitudes: A possible long-term proxy for the solar wind velocity?
title_full Dayside magnetic ULF power at high latitudes: A possible long-term proxy for the solar wind velocity?
title_fullStr Dayside magnetic ULF power at high latitudes: A possible long-term proxy for the solar wind velocity?
title_full_unstemmed Dayside magnetic ULF power at high latitudes: A possible long-term proxy for the solar wind velocity?
title_sort dayside magnetic ulf power at high latitudes: a possible long-term proxy for the solar wind velocity?
publishDate 1999
url https://orbit.dtu.dk/en/publications/6a9b2c47-68b8-47ba-b6e4-0aa385079fa7
genre Greenland
genre_facet Greenland
op_source Vennerstrøm , S 1999 , ' Dayside magnetic ULF power at high latitudes: A possible long-term proxy for the solar wind velocity? ' , Journal of Geophysical Research-space Physics , vol. 104 , no. A5 , pp. 10145-10157 .
op_relation https://orbit.dtu.dk/en/publications/6a9b2c47-68b8-47ba-b6e4-0aa385079fa7
op_rights info:eu-repo/semantics/restrictedAccess
_version_ 1810447577305317376