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Journal of Geophysical Research Atmospheres
Article . 1989 . Peer-reviewed
License: Wiley Online Library User Agreement
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Observations of motional electromagnetic fields during EMSLAB

Authors: Alan D. Chave; Jean H. Filloux; Douglas S. Luther; Lawrie K. Law; Antony White;

Observations of motional electromagnetic fields during EMSLAB

Abstract

The long‐period (>1 day) behavior of the seafloor electromagnetic fields during EMSLAB is considered in detail with an emphasis on interpretation in terms of oceanic motions. The study begins with a summary of the physics of motional electromagnetic induction, in which the seawater conductivity‐weighted, vertically integrated velocity measured by the horizontal electric field is emphasized. Using frequency‐domain methods, it is shown that seafloor and terrestrial magnetic variations have similar spectral shapes, indicating a common origin, but the seafloor electric field is not consistent with either at periods longer than 4 days, suggesting an oceanic source. The magnetic field variations are highly coherent across the EMSLAB array at periods shorter than 9 days, but the similarity decreases at longer periods, probably due to long‐term instrumental drift. The seafloor horizontal electric field data exhibit the broadband coherence characteristic of ionospheric sources only at periods shorter than 1–2 days and are essentially incoherent between 4 days and a week except in association with certain propagating wave phenomena. The distinction between the depth‐averaged velocity inferred from the horizontal electric field and its point measurement by the vertical electric field is demonstrated with data. Some specific properties of the seafloor electric fields are then considered in detail. The first of these is a 4‐day wave observed to propagate from north‐to‐south along the east flank of the Juan de Fuca Ridge. The wavelength, propagation sense, and association with the ridge are all consistent with topographically trapped Rossby wave behavior at a zero in the group velocity. A second north‐to‐south propagating wave is seen at periods of 8–12 days in the middle of the EMSLAB area with a probable wavelength of order 1000 km. Unresolved low‐frequency structures in the electric field are also mentioned. These observations clearly demonstrate the power of electromagnetic array methods for the study of long‐period oceanic behavior.

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selected citations
These citations are derived from selected sources.
This is an alternative to the "Influence" indicator, which also reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically).
BIP!Citations provided by BIP!
popularity
This indicator reflects the "current" impact/attention (the "hype") of an article in the research community at large, based on the underlying citation network.
BIP!Popularity provided by BIP!
influence
This indicator reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically).
BIP!Influence provided by BIP!
impulse
This indicator reflects the initial momentum of an article directly after its publication, based on the underlying citation network.
BIP!Impulse provided by BIP!
24
Average
Top 10%
Top 10%
bronze