College of Arts & Sciences
Physics can have some of the most unique and extraordinary applications of basic principles applied on a larger scale. This paper will explore the properties of induced magnetic dipoles and will examine this phenomenon directly from Jupiter's moon, Europa. These properties will be used to determine if there is liquid water beneath its icy surface and how this conclusion was verified. This will be accomplished using the concepts of magnetic dipoles and induced currents. Recent missions have also revealed estimates of the depth of Europa's subsurface ocean. There have been many measurements taken of Europa's magnetic field, and they are the most important variable in determining the depth of the Europan ocean depth. The relation between the magnetic dipole measurements and the ocean depth will be shown in figures.
Scholarly Commons Citation
Francis, L., & Zanolin, M. (2019). Induced Magnetic Dipole on Jupiter’s Moon Europa. , (). Retrieved from https://commons.erau.edu/student-works/84