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Open flux in Saturn’s magnetosphere

Open flux in Saturn’s magnetosphere
Open flux in Saturn’s magnetosphere
We characterise the interaction between the solar wind and Saturn’s magnetosphere by evaluating the amount of ‘open’ magnetic flux connected to the solar wind. This is deduced from a large set of Hubble Space Telescope images of the ultraviolet aurora, using the poleward boundary of the main aurora as a proxy for the open-closed field line boundary in the ionosphere. The amount of open flux is found to be 10–50 GWb, with a mean of 35 GWb. The typical change in open flux between consecutive observations separated by 10–60 h is -5-5 or +7 GWb. These changes are a result of imbalance between open flux creation at the dayside magnetopause and its closure in the magnetotail. The 5 GWb typical decrease in open flux is consistent with in situ measurements of the flux transported following a reconnection event. Estimates of average, net reconnection rates are found to be typically a few tens of kV, with some extreme examples of unbalanced magnetopause or tail reconnection occurring at ?300 kV. The range of values determined suggest that Saturn’s magnetosphere does not generally achieve a steady state between flux opening at the magnetopause and flux closure in the magnetotail. The percentage of magnetic flux which is open in Saturn’s magnetosphere is similar to that measured at the Earth (2–11%), but the typical percentage that is closed between observations is significantly lower (13% compared to 40–70%). Therefore, open flux is usually closed in smaller (few GWb) events in Saturn’s magnetosphere. The exception to this behaviour is large, rapid flux closure events which are associated with solar wind compressions. While the rates of flux opening and closure should be equal over long timescales, they are evidently different on shorter (up to tens of hours) timescales. The relative independence of the magnetopause and tail reconnection rates can be attributed to the long loading timescales required to transport open field lines into the tail
0019-1035
137-145
Badman, Sarah V.
a5cd5518-6896-4cfb-b8d6-56293aa8c825
Jackman, Caitriona
9bc3456c-b254-48f1-ade0-912c5b8b4529
Nichols, Jonathan D.
d355c18a-4a5e-4d0f-a8f4-d32efa4b5128
Clarke, John T.
4a4389b6-32da-45ca-805b-bc51d3d90398
Gérard, Jean-Claude
7b1935e9-8fd1-4b22-af81-4ff47eca1c63
Badman, Sarah V.
a5cd5518-6896-4cfb-b8d6-56293aa8c825
Jackman, Caitriona
9bc3456c-b254-48f1-ade0-912c5b8b4529
Nichols, Jonathan D.
d355c18a-4a5e-4d0f-a8f4-d32efa4b5128
Clarke, John T.
4a4389b6-32da-45ca-805b-bc51d3d90398
Gérard, Jean-Claude
7b1935e9-8fd1-4b22-af81-4ff47eca1c63

Badman, Sarah V., Jackman, Caitriona, Nichols, Jonathan D., Clarke, John T. and Gérard, Jean-Claude (2014) Open flux in Saturn’s magnetosphere. Icarus, 231, 137-145. (doi:10.1016/j.icarus.2013.12.004).

Record type: Article

Abstract

We characterise the interaction between the solar wind and Saturn’s magnetosphere by evaluating the amount of ‘open’ magnetic flux connected to the solar wind. This is deduced from a large set of Hubble Space Telescope images of the ultraviolet aurora, using the poleward boundary of the main aurora as a proxy for the open-closed field line boundary in the ionosphere. The amount of open flux is found to be 10–50 GWb, with a mean of 35 GWb. The typical change in open flux between consecutive observations separated by 10–60 h is -5-5 or +7 GWb. These changes are a result of imbalance between open flux creation at the dayside magnetopause and its closure in the magnetotail. The 5 GWb typical decrease in open flux is consistent with in situ measurements of the flux transported following a reconnection event. Estimates of average, net reconnection rates are found to be typically a few tens of kV, with some extreme examples of unbalanced magnetopause or tail reconnection occurring at ?300 kV. The range of values determined suggest that Saturn’s magnetosphere does not generally achieve a steady state between flux opening at the magnetopause and flux closure in the magnetotail. The percentage of magnetic flux which is open in Saturn’s magnetosphere is similar to that measured at the Earth (2–11%), but the typical percentage that is closed between observations is significantly lower (13% compared to 40–70%). Therefore, open flux is usually closed in smaller (few GWb) events in Saturn’s magnetosphere. The exception to this behaviour is large, rapid flux closure events which are associated with solar wind compressions. While the rates of flux opening and closure should be equal over long timescales, they are evidently different on shorter (up to tens of hours) timescales. The relative independence of the magnetopause and tail reconnection rates can be attributed to the long loading timescales required to transport open field lines into the tail

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Accepted/In Press date: 5 December 2013
e-pub ahead of print date: 12 December 2013
Published date: 1 March 2014
Organisations: Astronomy Group

Identifiers

Local EPrints ID: 401234
URI: http://eprints.soton.ac.uk/id/eprint/401234
ISSN: 0019-1035
PURE UUID: 8a47348a-996d-4eee-803b-eb462b13f422
ORCID for Caitriona Jackman: ORCID iD orcid.org/0000-0003-0635-7361

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Date deposited: 10 Oct 2016 10:44
Last modified: 15 Mar 2024 02:42

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Contributors

Author: Sarah V. Badman
Author: Jonathan D. Nichols
Author: John T. Clarke
Author: Jean-Claude Gérard

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