Criterion for interchange instability in a plasma connected to a conducting ionosphere

Details Criterion for interchange instability in a plasma connected to a conducting ionosphere Criterion for interchange instability in a plasma connected to a conducting ionosphere

Dec 2007

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007jgra..11212209x&link_type=abstract

Journal of Geophysical Research, Volume 112, Issue A12, CiteID A12209

Physics

13

Magnetospheric Physics: Plasma Sheet, Magnetospheric Physics: Plasma Waves And Instabilities (2471), Magnetospheric Physics: Magnetosphere: Inner, Magnetospheric Physics: Magnetosphere/Ionosphere Interactions (2431)

Scientific paper

We have combined two empirical numerical models to estimate the entropy parameter PV 5/3 in the plasma sheet, where P is the plasma sheet pressure and V = ∫$\frac{ds}{B is the volume of a flux tube containing one unit of magnetic flux. The Tsyganenko and Stern (1996) magnetic field model is used to calculate the flux tube volume, and the Tsyganenko and Mukai (2003) plasma sheet statistical model is used to calculate the plasma sheet pressure. Contour plots for PV 5/3 and V in the equatorial plane are presented for various solar wind conditions. These empirical models suggest that, although both PV 5/3 and V generally increase tailward, their gradients are generally not parallel or antiparallel to each other, whereas most theoretical discussions of interchange instability assume that the vectors are lined up. The Vasyliunas equation implies that the Birkeland current is proportional to the cross product of $\nabla$ PV 5/3 and $\nabla$ V, so that region 1 and region 2 Birkeland current flow between plasma sheet and ionosphere confirms that the gradients of entropy parameter and flux tube volume are not generally parallel. We present analytical calculations to investigate the criterion for interchange instability in a quasi-static, low-β plasma that is connected to a conducting ionosphere and has $\nabla$ PV 5/3 and $\nabla$ V at an arbitrary angle α, which implies shear flows. A boundary layer is assumed to separate two regions with different but uniform PV 5/3. The main conclusion is that the system is interchange unstable if α > π/2. The results suggest that the statistical average plasma sheet configuration is interchange stable since the statistical plasma sheet models indicate that α < π/2. Our conclusion is quite different from analyses that neglect shear flow since they imply instability unless $\nabla$ PV 5/3 and $\nabla$ V are exactly parallel.

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