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The electric current vector is superposed on each color contour.
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The energy the magnetosphere is gaining from the solar wind for magnetospheric substorms and storms can be estimated from the distribution of electric current vectors in space, which are obtained from geomagnetic disturbances observed on the ground.
The large arrows indicate representative induced electric currents (purple vectors) and secondary induced magnetic fields (red arcs) 1 First motion The flow of the first tsunami wave was more than 100 km northeast of Chichijima Island.
The direction of the electric current is estimated by computing the flow velocity vectors.
Magnetic field, a vector field in the neighbourhood of a magnet, electric current, or changing electric field, in which magnetic forces are observable.
We utilize the high-cadence, high-resolution vector magnetograms observed by Big Bear Solar Observatory (BBSO) to derive the longitudinal electric current and analyze the distribution of the longitudinal electric current in the region of sunspots, and simulate the distributing features of the solar plasma loops.
Through combining the definition of electric current as the time rate of change of electric charge, a rule of vector multiplication called Lorentz's Law describes the force on a charge moving in a magnetic field.
Using the Maxwell equation for current density j, this electric current is determined by mu boldsymbol{j}=nabla times boldsymbol{b}, where μ is the magnetic permeability and j is the vector of current density.
The measured magnetic field from Big Bear Solar Observatory (BBSO) digital vector magnetograph (DGVM) was used to model the non-potential coronal magnetic field changes and the evolution of electric current before and after the event occurred.
See also electric current.
See electric current.
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