Solar wind-magnetosphere energy input functions
L. F. Bargatze, R. L. McPherron, D. N. Baker
Department of Earth and Space Sciences, University of California, Los Angeles, CA 90024
Abstract:
A new formula for the solar wind-magnetosphere energy input parameter, Pi, is sought by applying the constraints imposed by dimensional analysis. Applying these constraints yields a general equations for Pi which is equal to r V3l2CF(MA,q ) where, r V3 is the solar wind kinetic energy density and l2CF is the scale size of the magnetosphere's effective energy "collection" region. The function F which depends on MA, the Alfvén Mach number, and on q , the interplanetary magnetic field clock angle is included in the general equation for Pi in order to model the magnetohydrodynamic processes which are responsible for solar wind-magnetosphere energy transfer. By assuming the form of the function F, it is possible to further constrain the formula for Pi. This is accomplished by using solar wind data, geomagnetic activity indices, and simple statistical methods. It is found that Pi is proportional to (r V2)1/6VBG(q ) where, r V2 is the solar wind dynamic pressure and VBG(q ) is a rectified version of the solar wind motional electric field. Furthermore, it is found that G(q ), the gating function which modulates the energy input to the magnetosphere, is well represented by a "leaky" rectifier functions such as sin4(q / 2). This function allows for enhanced energy input when the interplanetary magnetic field is oriented southward. This function also allows for some energy input when the interplanetary magnetic field is oriented northward.
in Solar Wind-Magnetosphere Coupling, edited by Y. Kamide and J. A. Slavin, pp. 101-110, Terra Scient. Publ. Co., Tokyo, 1986