An accelerating high-latitude jet in Earth’s core

Philip W. Livermore, Rainer Hollerbach, Chris Finlay

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Abstract

Observations of the change in Earth’s magnetic field—the secular variation—provide information about the motion of liquid metal within the core that is responsible for the magnetic field’s generation. High-resolution observations from the European Space Agency’s Swarm satellite mission show intense field change at high latitude, localized in a distinctive circular daisy-chain configuration centred on the north geographic pole. Here we show that this feature can be explained by a localized, non-axisymmetric, westward jet of 420 km width on the tangent cylinder, the cylinder of fluid within the core that is aligned with the rotation axis and tangent to the solid inner core. We find that the jet has increased in magnitude by a factor of three over the period 2000–2016 to about 40 km yr−1, and is now much stronger than typical large-scale flows inferred for the core. We suggest that the current accelerating phase may be part of a longer-term fluctuation of the jet causing both eastward and westward movement of magnetic features over historical periods, and may contribute to recent changes in torsional-wave activity and the rotation direction of the inner core.
Original languageEnglish
JournalNature Geoscience
Volume10
Issue number1
Pages (from-to)62-68
ISSN1752-0894
DOIs
Publication statusPublished - 2016

Cite this

W. Livermore, Philip ; Hollerbach, Rainer ; Finlay, Chris. / An accelerating high-latitude jet in Earth’s core. In: Nature Geoscience. 2016 ; Vol. 10, No. 1. pp. 62-68.
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An accelerating high-latitude jet in Earth’s core. / W. Livermore, Philip; Hollerbach, Rainer; Finlay, Chris.

In: Nature Geoscience, Vol. 10, No. 1, 2016, p. 62-68.

Research output: Contribution to journalJournal articleResearchpeer-review

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AU - W. Livermore, Philip

AU - Hollerbach, Rainer

AU - Finlay, Chris

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AB - Observations of the change in Earth’s magnetic field—the secular variation—provide information about the motion of liquid metal within the core that is responsible for the magnetic field’s generation. High-resolution observations from the European Space Agency’s Swarm satellite mission show intense field change at high latitude, localized in a distinctive circular daisy-chain configuration centred on the north geographic pole. Here we show that this feature can be explained by a localized, non-axisymmetric, westward jet of 420 km width on the tangent cylinder, the cylinder of fluid within the core that is aligned with the rotation axis and tangent to the solid inner core. We find that the jet has increased in magnitude by a factor of three over the period 2000–2016 to about 40 km yr−1, and is now much stronger than typical large-scale flows inferred for the core. We suggest that the current accelerating phase may be part of a longer-term fluctuation of the jet causing both eastward and westward movement of magnetic features over historical periods, and may contribute to recent changes in torsional-wave activity and the rotation direction of the inner core.

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