This current interacts with the magnetic flux to produce a counterclockwise torque, which in turn accelerates the rotor.
Sea-level changes and ocean current interacted during the evolution of the carbonate platforms, and one or the other factor determined the major changeovers in the platform evolution.
When a potential difference is applied across pairs or groups of electrodes, the resulting current interacts with the magnetic field to induce Lorentz forces and fluid motion.
Here we show, by means of numerical simulations, how a dilute pyroclastic density current interacts with four different types of simple topography, namely: flat, one hill, one valley and two hills.
The channel has a constant width denoted as W. The lock region is initially at rest with density ρ 1, chosen such that ρ B > ρ 1 > ρ T. At t=0, the lock is released and the particle-laden flow moves down the slope forming a turbidity current interacting with the ambient fluid.
When this current interacts with the northeastern coast of South America, the current forks into two branches.
The radial current interacts with the planetary magnetic field, and the resulting Lorentz force accelerates the magnetospheric plasma in the direction of planetary rotation.
Most of those features only describe current interacting residues, but cannot represent real situation well, thus are insufficient to predict binding sites with high accuracy.
Some features only describe properties of current interacting residues, but cannot represent real situation well, thus are insufficient to predict binding sites with high accuracy.
In energetic areas, waves and tidal currents interact for modifying the energy resource and impacting on the design conditions.
