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Increases in plasma sheet temperature with solar wind driving during substorm growth phases

During substorm growth phases, magnetic reconnection at the magnetopause extracts ∼10(15) J from the solar wind which is then stored in the magnetotail lobes. Plasma sheet pressure increases to balance magnetic flux density increases in the lobes. Here we examine plasma sheet pressure, density, and...

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Detalles Bibliográficos
Autores principales: Forsyth, C, Watt, C E J, Rae, I J, Fazakerley, A N, Kalmoni, N M E, Freeman, M P, Boakes, P D, Nakamura, R, Dandouras, I, Kistler, L M, Jackman, C M, Coxon, J C, Carr, C M
Formato: Online Artículo Texto
Lenguaje:English
Publicado: BlackWell Publishing Ltd 2014
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4459207/
https://www.ncbi.nlm.nih.gov/pubmed/26074645
http://dx.doi.org/10.1002/2014GL062400
Descripción
Sumario:During substorm growth phases, magnetic reconnection at the magnetopause extracts ∼10(15) J from the solar wind which is then stored in the magnetotail lobes. Plasma sheet pressure increases to balance magnetic flux density increases in the lobes. Here we examine plasma sheet pressure, density, and temperature during substorm growth phases using 9 years of Cluster data (>316,000 data points). We show that plasma sheet pressure and temperature are higher during growth phases with higher solar wind driving, whereas the density is approximately constant. We also show a weak correlation between plasma sheet temperature before onset and the minimum SuperMAG AL (SML) auroral index in the subsequent substorm. We discuss how energization of the plasma sheet before onset may result from thermodynamically adiabatic processes; how hotter plasma sheets may result in magnetotail instabilities, and how this relates to the onset and size of the subsequent substorm expansion phase.