The dependence of magnetic reconnection on plasma β and magnetic shear: Evidence from magnetopause observations

We have performed a statistical study of THEMIS spacecraft crossings of the asymmetric dayside magnetopause to test the prediction that the diamagnetic drift of the X-line due to a plasma pressure gradient across the magnetopause can suppress magnetic reconnection. The study includes crossings both when reconnection exhausts were present and when they were absent in the current sheet. When we restrict the survey to the subsolar region (10 < MLT < 14), we find that for low Delta beta (the difference of plasma beta on the two sides of the current sheet) the majority of reconnection events occurred over a large range of magnetic shears, whereas when Delta beta was high reconnection events occurred only for high shears. Furthermore, nonreconnection events occurred primarily in the Delta beta-shear regime in which reconnection is predicted to be suppressed, in good agreement with theory. The Delta beta-shear condition should have general consequences for the occurrence of reconnection in space and laboratory plasmas. Citation: Phan, T. D., G. Paschmann, J. T. Gosling, M. Oieroset, M. Fujimoto, J. F. Drake, and V. Angelopoulos (2013), The dependence of magnetic reconnection on plasma beta and magnetic shear: Evidence from magnetopause observations, Geophys. Res. Lett., 40, 11-16, doi: 10.1029/2012GL054528.