Articles | Volume 14, issue 3
Ocean Sci., 14, 515–524, 2018
https://doi.org/10.5194/os-14-515-2018
Ocean Sci., 14, 515–524, 2018
https://doi.org/10.5194/os-14-515-2018

Research article 25 Jun 2018

Research article | 25 Jun 2018

Electromagnetic characteristics of ENSO

Johannes Petereit et al.

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Cited articles

Bamston, A. G., Chelliah, M., and Goldenberg, S. B.: Documentation of a highly ENSO related SST region in the equatorial Pacific: Research note, Atmos. Ocean, 35, 367–383, 1997. a
Chave, A. D. and Luther, D. S.: Low-frequency, motionally induced electromagnetic fields in the ocean: 1. Theory, J. Geophys. Res.-Oceans, 95, 7185–7200, 1990. a
Egbert, G. D. and Erofeeva, S. Y.: Efficient inverse modeling of barotropic ocean tides, J. Atmos. Ocean. Tech., 19, 183–204, 2002. a
Egbert, G. D., Bennett, A. F., and Foreman, M. G.: TOPEX/POSEIDON tides estimated using a global inverse model, J. Geophys. Res.-Oceans, 99, 24821–24852, 1994. a
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Short summary
The study finds that changes in seawater temperature due to El Niño and La Niña, anomalous warm and cold events, are in principle detectable by means of the oceanic tidally induced magnetic field. Furthermore, subsurface processes in the onset of those anomalous events lead the surface processes by several months. This causes a lead in the oceanic tidally induced magnetic field signals over sea-surface temperature signals.