Sentence examples for field diffusion from inspiring English sources

Figure 6 Effects of the toroidal field diffusion.

Amit and Christensen ([2008]) find in numerical dynamos that poloidal field diffusion is roughly evenly distributed at all latitudes.

The time-domain finite-difference method has been widely used in simulation of the electromagnetic field diffusion.

Experimental success is mainly attributed to careful identification of local magnetic field diffusion time-constants, and individual actuator channel peripheral dynamics.

However, if poloidal field diffusion should also be concentrated at low latitude in the geomagnetic field, core flow inversions from geomagnetic secular variation may be affected, in particular, at low latitude (Amit and Christensen [2008]).

This new approach is validated with standard analytical solutions for planar magnetic flux compression system and magnetic field diffusion in moving conductors with a non-relativistic velocity.

These observations indicate that the particles undergo a significant cross-field diffusion.

Large small-scale gradients normal to the local magnetic field are shown to be completely consistent with significant cross-field diffusion on larger time scales.

Phase space distributions from the simulation technique for various low mass ions are compared with SWICS and HI-SCALE data to deduce values of a "turbulence parameter" that controls the efficiency of injection, and the degree of cross-field diffusion.

The magnetic field strength, shell size and degree of particle cross-field diffusion act as variables to which the radio to X-ray to gamma-ray signal is sensitive.

We attribute the fact that the decay phases of these events are nearly the same at Ulysses and in the ecliptic rather to cross-field diffusion than to the presence of a shock.