Open AccessSatellite magnetic data reveal interannual waves in Earth’s core
Author(s) -
Nicolas Gillet,
Felix Gerick,
D. Jault,
Tobias Schwaiger,
Julien Aubert,
Mathieu Istas
Publication year - 2022
Publication title -
proceedings of the national academy of sciences of the united states of america
Language(s) - English
Resource type - Journals
eISSN - 1091-6490
pISSN - 0027-8424
DOI - 10.1073/pnas.2115258119
Subject(s) - satellite , earth (classical element) , core (optical fiber) , remote sensing , geology , geophysics , computer science , physics , telecommunications , astronomy
Significance The physics responsible for most of the interannual geomagnetic field changes, continually recorded by satellites for 20 years, is a long-standing open issue. By analyzing magnetic data, we detect Magneto–Coriolis waves in the Earth’s outer core that account for a significant part of this signal. We further propose theoretical advances in the physical characterization of these waves, enabling a deeper understanding of the dynamics behind the geomagnetic signal. It should allow one to better sketch the heterogeneous magnetic field deep within the core, shedding further light on the mechanisms that sustain the geodynamo. Our interpretation does not require the presence of a stratified layer at the top of the core, with potent consequences regarding the Earth’s thermal history.