Step 1: Understanding upward continuation.
Upward continuation is a mathematical transformation applied to potential field data (e.g., magnetic or gravity data) to simulate measurements at a higher elevation than the actual observation level.
Step 2: Effects on magnetic sources. It reduces the influence of shallow magnetic sources because their field strength decays rapidly with height.
In contrast, it relatively enhances the contribution from deeper sources, as their field strength decays more slowly.
Step 3: Eliminating incorrect options.
(C) is incorrect because upward continuation suppresses, rather than enhances, near-surface anomalies.
(D) is incorrect; it’s a misinterpretation — sources do not move, only their apparent influence changes.
A current-carrying coil is placed in an external uniform magnetic field. The coil is free to turn in the magnetic field. What is the net force acting on the coil? Obtain the orientation of the coil in stable equilibrium. Show that in this orientation the flux of the total field (field produced by the loop + external field) through the coil is maximum.