Global observations of magnetospheric high-m poloidal waves during the 22 June 2015 magnetic storm

We report global observations of high-m poloidal waves during the recovery phase of the 22 June 2015 magnetic storm from a constellation of widely spaced satellites of five missions including Magnetospheric Multiscale (MMS), Van Allen Probes, Time History of Events and Macroscale Interactions during...

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Veröffentlicht in:Geophysical research letters. - 1984. - 44(2017), 8 vom: 28. Apr., Seite 3456-3464
1. Verfasser: Le, G (VerfasserIn)
Weitere Verfasser: Chi, P J, Strangeway, R J, Russell, C T, Slavin, J A, Takahashi, K, Singer, H J, Anderson, B J, Bromund, K, Fischer, D, Kepko, E L, Magnes, W, Nakamura, R, Plaschke, F, Torbert, R B
Format: Online-Aufsatz
Sprache:English
Veröffentlicht: 2017
Zugriff auf das übergeordnete Werk:Geophysical research letters
Schlagworte:Journal Article ULF waves field line resonances high‐m poloidal waves magnetic storm magnetospheric multiscale mission
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520 |a We report global observations of high-m poloidal waves during the recovery phase of the 22 June 2015 magnetic storm from a constellation of widely spaced satellites of five missions including Magnetospheric Multiscale (MMS), Van Allen Probes, Time History of Events and Macroscale Interactions during Substorm (THEMIS), Cluster, and Geostationary Operational Environmental Satellites (GOES). The combined observations demonstrate the global spatial extent of storm time poloidal waves. MMS observations confirm high azimuthal wave numbers (m ~ 100). Mode identification indicates the waves are associated with the second harmonic of field line resonances. The wave frequencies exhibit a decreasing trend as L increases, distinguishing them from the single-frequency global poloidal modes normally observed during quiet times. Detailed examination of the instantaneous frequency reveals discrete spatial structures with step-like frequency changes along L. Each discrete L shell has a steady wave frequency and spans about 1 RE , suggesting that there exist a discrete number of drift-bounce resonance regions across L shells during storm times 
650 4 |a Journal Article 
650 4 |a ULF waves 
650 4 |a field line resonances 
650 4 |a high‐m poloidal waves 
650 4 |a magnetic storm 
650 4 |a magnetospheric multiscale mission 
700 1 |a Chi, P J  |e verfasserin  |4 aut 
700 1 |a Strangeway, R J  |e verfasserin  |4 aut 
700 1 |a Russell, C T  |e verfasserin  |4 aut 
700 1 |a Slavin, J A  |e verfasserin  |4 aut 
700 1 |a Takahashi, K  |e verfasserin  |4 aut 
700 1 |a Singer, H J  |e verfasserin  |4 aut 
700 1 |a Anderson, B J  |e verfasserin  |4 aut 
700 1 |a Bromund, K  |e verfasserin  |4 aut 
700 1 |a Fischer, D  |e verfasserin  |4 aut 
700 1 |a Kepko, E L  |e verfasserin  |4 aut 
700 1 |a Magnes, W  |e verfasserin  |4 aut 
700 1 |a Nakamura, R  |e verfasserin  |4 aut 
700 1 |a Plaschke, F  |e verfasserin  |4 aut 
700 1 |a Torbert, R B  |e verfasserin  |4 aut 
773 0 8 |i Enthalten in  |t Geophysical research letters  |d 1984  |g 44(2017), 8 vom: 28. Apr., Seite 3456-3464  |w (DE-627)NLM098182501  |x 0094-8276  |7 nnns 
773 1 8 |g volume:44  |g year:2017  |g number:8  |g day:28  |g month:04  |g pages:3456-3464 
856 4 0 |u http://dx.doi.org/10.1002/2017GL073048  |3 Volltext 
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