kjernefeltmodeller
Kjernefeltmodeller, often translated as "core field models" or "kernel field models," are theoretical frameworks used in various scientific disciplines, particularly in physics and geophysics, to describe phenomena dominated by a central, powerful source or field. These models often simplify complex systems by assuming that the most significant interactions originate from a core region, and the effects at a distance are a consequence of this central influence.
In geophysics, kjernefeltmodeller are frequently employed to understand the Earth's magnetic field. The geodynamo theory suggests
Beyond Earth sciences, the concept of kjernefeltmodeller can be applied to other areas where a central source