Abstract

The coefficient of magnetohydrodynamic(MHD)eddyviscosity of the turbulentsolar wind is calculated to be νeddy≈1.3×1017cm2/s: this coefficient is appropriate for velocity shears with scale thicknesses larger than the ∼106 km correlation length of the solar-windturbulence. The coefficient of MHDeddyviscosity is calculated again accounting for the action of smaller-scale turbulenteddies on smaller scale velocity shears in the solar wind. This eddyviscosity is quantitatively tested with spacecraft observations of shear flows in co-rotating interaction regions (CIRs) and in coronal-mass-ejection (CME) sheaths and ejecta. It is found that the large-scale (∼107km) shear of the CIR fractures into intense narrow (∼105km) slip zones between slabs of differently magnetized plasma. Similarly, it is found that the large-scale shear of CME sheaths also fracture into intense narrow slip zones between parcels of differently magnetized plasma. Using the solar-wind eddy-viscosity coefficient to calculate vorticity-diffusion time scales and comparing those time scales with the ∼100-h age of the solar-wind plasma at 1AU, it is found that the slip zones are much narrower than eddy-viscosity theory says they should be. Thus, our concept of MHDeddyviscosity fails testing. For the freestream turbulence effect in solar-windmagnetosphere coupling, the eddy-viscous force of the solar wind on the Earth's magnetosphere is rederived accounting for the action of turbulenteddies smaller than the correlation length, along with other corrections. The improved derivation of the solar-wind driver function for the turbulence effect fails to yield higher correlation coefficients between measurements of the solar-wind driver and measurements of the response of the Earth's magnetosphere.