Geomagnetic jerks and rapid hydromagnetic waves focusing at Earth's core surface

Julien Aubert*, Christopher C. Finlay

*Corresponding author for this work

Research output: Contribution to journalJournal articleResearchpeer-review

Abstract

Geomagnetic jerks are abrupt changes in the second time derivative-the secular acceleration-of Earth's magnetic field that punctuate ground observatory records. As their dynamical origin has not yet been established, they represent a major obstacle to the prediction of geomagnetic field behaviour for years to decades ahead. Recent jerks have been linked to short-lived, temporally alternating and equatorially localized pulses of secular acceleration observed in satellite data, associated with rapidly alternating flows at Earth's core surface. Here we show that these signatures can be reproduced in numerical simulations of the geodynamo that realistically account for the interaction between slow core convection and rapid hydromagnetic waves. In these simulations, jerks are caused by the arrival of localized Alfven wave packets radiated from sudden buoyancy releases inside the core. As they reach the core surface, the waves focus their energy towards the equatorial plane and along lines of strong magnetic flux, creating sharp interannual changes in core flow and producing geomagnetic jerks through the induced variations in magnetic field acceleration. The ability to numerically reproduce jerks offers a new way to probe the physical properties of Earth's deep interior.
Original languageEnglish
JournalNature Geoscience
Volume12
Issue number5
Pages (from-to)393–398
ISSN1752-0894
DOIs
Publication statusPublished - 2019

Cite this

@article{230667cf919d4619bfb41edaa2ca5ba3,
title = "Geomagnetic jerks and rapid hydromagnetic waves focusing at Earth's core surface",
abstract = "Geomagnetic jerks are abrupt changes in the second time derivative-the secular acceleration-of Earth's magnetic field that punctuate ground observatory records. As their dynamical origin has not yet been established, they represent a major obstacle to the prediction of geomagnetic field behaviour for years to decades ahead. Recent jerks have been linked to short-lived, temporally alternating and equatorially localized pulses of secular acceleration observed in satellite data, associated with rapidly alternating flows at Earth's core surface. Here we show that these signatures can be reproduced in numerical simulations of the geodynamo that realistically account for the interaction between slow core convection and rapid hydromagnetic waves. In these simulations, jerks are caused by the arrival of localized Alfven wave packets radiated from sudden buoyancy releases inside the core. As they reach the core surface, the waves focus their energy towards the equatorial plane and along lines of strong magnetic flux, creating sharp interannual changes in core flow and producing geomagnetic jerks through the induced variations in magnetic field acceleration. The ability to numerically reproduce jerks offers a new way to probe the physical properties of Earth's deep interior.",
author = "Julien Aubert and Finlay, {Christopher C.}",
year = "2019",
doi = "10.1038/s41561-019-0355-1",
language = "English",
volume = "12",
pages = "393–398",
journal = "Nature Geoscience",
issn = "1752-0894",
publisher = "Nature Publishing Group",
number = "5",

}

Geomagnetic jerks and rapid hydromagnetic waves focusing at Earth's core surface. / Aubert, Julien; Finlay, Christopher C.

In: Nature Geoscience, Vol. 12, No. 5, 2019, p. 393–398.

Research output: Contribution to journalJournal articleResearchpeer-review

TY - JOUR

T1 - Geomagnetic jerks and rapid hydromagnetic waves focusing at Earth's core surface

AU - Aubert, Julien

AU - Finlay, Christopher C.

PY - 2019

Y1 - 2019

N2 - Geomagnetic jerks are abrupt changes in the second time derivative-the secular acceleration-of Earth's magnetic field that punctuate ground observatory records. As their dynamical origin has not yet been established, they represent a major obstacle to the prediction of geomagnetic field behaviour for years to decades ahead. Recent jerks have been linked to short-lived, temporally alternating and equatorially localized pulses of secular acceleration observed in satellite data, associated with rapidly alternating flows at Earth's core surface. Here we show that these signatures can be reproduced in numerical simulations of the geodynamo that realistically account for the interaction between slow core convection and rapid hydromagnetic waves. In these simulations, jerks are caused by the arrival of localized Alfven wave packets radiated from sudden buoyancy releases inside the core. As they reach the core surface, the waves focus their energy towards the equatorial plane and along lines of strong magnetic flux, creating sharp interannual changes in core flow and producing geomagnetic jerks through the induced variations in magnetic field acceleration. The ability to numerically reproduce jerks offers a new way to probe the physical properties of Earth's deep interior.

AB - Geomagnetic jerks are abrupt changes in the second time derivative-the secular acceleration-of Earth's magnetic field that punctuate ground observatory records. As their dynamical origin has not yet been established, they represent a major obstacle to the prediction of geomagnetic field behaviour for years to decades ahead. Recent jerks have been linked to short-lived, temporally alternating and equatorially localized pulses of secular acceleration observed in satellite data, associated with rapidly alternating flows at Earth's core surface. Here we show that these signatures can be reproduced in numerical simulations of the geodynamo that realistically account for the interaction between slow core convection and rapid hydromagnetic waves. In these simulations, jerks are caused by the arrival of localized Alfven wave packets radiated from sudden buoyancy releases inside the core. As they reach the core surface, the waves focus their energy towards the equatorial plane and along lines of strong magnetic flux, creating sharp interannual changes in core flow and producing geomagnetic jerks through the induced variations in magnetic field acceleration. The ability to numerically reproduce jerks offers a new way to probe the physical properties of Earth's deep interior.

U2 - 10.1038/s41561-019-0355-1

DO - 10.1038/s41561-019-0355-1

M3 - Journal article

VL - 12

SP - 393

EP - 398

JO - Nature Geoscience

JF - Nature Geoscience

SN - 1752-0894

IS - 5

ER -