A gyroviscous model of the magnetotail current layer and the substorm mechanism
DOI10.1063/1.866253zbMath0623.76138OpenAlexW2001228872MaRDI QIDQ3762019
Publication date: 1987
Published in: The Physics of Fluids (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1063/1.866253
momentum equationHall currentnecessary conditionmagnetospheregeneralized Ohm's lawself-consistent solutionsmagnetospheric substormsfinite ion Larmor radiuscollision-free plasmascross-equatorial mass transportdynamically stable configurationgyroviscous stressesisotropic scalar pressuremagnetotail current layerone-dimensional current layerplasma flow vector
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