Momentum transfer at the high-latitude magnetopause and boundary layers

How and where momentum is transferred from the solar wind to the magnetosphere and ionosphere is one of the key problems of space physics. Much of this transfer occurs through direct reconnection on the dayside, particularly when the IMF is southward. However, momentum transfer also occurs at hi...

Full description

Bibliographic Details
Main Authors: E. J. Lund, C. J. Farrugia, P. E. Sandholt
Format: Article
Language:English
Published: Copernicus Publications 2008-08-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/26/2449/2008/angeo-26-2449-2008.pdf
id doaj-41bf0318c1664542a7432163d3abadbf
record_format Article
spelling doaj-41bf0318c1664542a7432163d3abadbf2020-11-25T00:29:55ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762008-08-01262449245810.5194/angeo-26-2449-2008Momentum transfer at the high-latitude magnetopause and boundary layersE. J. Lund0C. J. Farrugia1P. E. Sandholt2Space Science Center, University of New Hampshire, Durham, New Hampshire, USASpace Science Center, University of New Hampshire, Durham, New Hampshire, USADepartment of Physics, University of Oslo, Oslo, NorwayHow and where momentum is transferred from the solar wind to the magnetosphere and ionosphere is one of the key problems of space physics. Much of this transfer occurs through direct reconnection on the dayside, particularly when the IMF is southward. However, momentum transfer also occurs at higher latitudes via Alfvén waves on old open field lines, even for southward IMF. This momentum is transferred to the ionosphere via field-aligned currents (FACs), and the flow channel associated with these FACs produces a Hall current which causes magnetic variations at high latitude (the Svalgaard-Mansurov effect). We show examples where such momentum transfer is observed with multiple spacecraft and ground-based instruments.https://www.ann-geophys.net/26/2449/2008/angeo-26-2449-2008.pdf
collection DOAJ
language English
format Article
sources DOAJ
author E. J. Lund
C. J. Farrugia
P. E. Sandholt
spellingShingle E. J. Lund
C. J. Farrugia
P. E. Sandholt
Momentum transfer at the high-latitude magnetopause and boundary layers
Annales Geophysicae
author_facet E. J. Lund
C. J. Farrugia
P. E. Sandholt
author_sort E. J. Lund
title Momentum transfer at the high-latitude magnetopause and boundary layers
title_short Momentum transfer at the high-latitude magnetopause and boundary layers
title_full Momentum transfer at the high-latitude magnetopause and boundary layers
title_fullStr Momentum transfer at the high-latitude magnetopause and boundary layers
title_full_unstemmed Momentum transfer at the high-latitude magnetopause and boundary layers
title_sort momentum transfer at the high-latitude magnetopause and boundary layers
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2008-08-01
description How and where momentum is transferred from the solar wind to the magnetosphere and ionosphere is one of the key problems of space physics. Much of this transfer occurs through direct reconnection on the dayside, particularly when the IMF is southward. However, momentum transfer also occurs at higher latitudes via Alfvén waves on old open field lines, even for southward IMF. This momentum is transferred to the ionosphere via field-aligned currents (FACs), and the flow channel associated with these FACs produces a Hall current which causes magnetic variations at high latitude (the Svalgaard-Mansurov effect). We show examples where such momentum transfer is observed with multiple spacecraft and ground-based instruments.
url https://www.ann-geophys.net/26/2449/2008/angeo-26-2449-2008.pdf
work_keys_str_mv AT ejlund momentumtransferatthehighlatitudemagnetopauseandboundarylayers
AT cjfarrugia momentumtransferatthehighlatitudemagnetopauseandboundarylayers
AT pesandholt momentumtransferatthehighlatitudemagnetopauseandboundarylayers
_version_ 1725329007979790336