Signatures of High‐Latitude Waves in Observations of Geomagnetic Acceleration

Abstract Models for the second time‐derivative of the geomagnetic field reveal prominent activity at high latitudes. Alternating patches of positive and negative geomagnetic acceleration propagate to the west at speeds that exceed nominal fluid velocities in the core. We show that waves are a viable...

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Main Authors: Rodrigo Chi‐Durán, Margaret S. Avery, Bruce A. Buffett
Format: Article
Language:English
Published: Wiley 2021-10-01
Series:Geophysical Research Letters
Online Access:https://doi.org/10.1029/2021GL094692
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author Rodrigo Chi‐Durán
Margaret S. Avery
Bruce A. Buffett
author_facet Rodrigo Chi‐Durán
Margaret S. Avery
Bruce A. Buffett
author_sort Rodrigo Chi‐Durán
collection DOAJ
description Abstract Models for the second time‐derivative of the geomagnetic field reveal prominent activity at high latitudes. Alternating patches of positive and negative geomagnetic acceleration propagate to the west at speeds that exceed nominal fluid velocities in the core. We show that waves are a viable interpretation of these observations. Magnetic Rossby waves produce a high‐latitude response with suitable phase velocities. However, the spatial complexity of the prediction is not compatible with the observations. Our preferred interpretation involves zonal MAC waves. These waves can account for the observed geomagnetic field when a stratified layer exists at the top of the core. The required layer has a thickness in excess of 100 km and a buoyancy frequency comparable to the rotation frequency. We anticipate a gradual reduction in the phase velocity over time, leading to a future change in the propagation direction.
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series Geophysical Research Letters
spelling doaj-art-81b06c2971ec4fc6975c7350defd26cf2025-08-20T02:09:35ZengWileyGeophysical Research Letters0094-82761944-80072021-10-014820n/an/a10.1029/2021GL094692Signatures of High‐Latitude Waves in Observations of Geomagnetic AccelerationRodrigo Chi‐Durán0Margaret S. Avery1Bruce A. Buffett2Department of Earth and Planetary Science University of California, Berkeley Berkeley CA USAU.S. Geological Survey, Moffett Field Menlo Park CA USADepartment of Earth and Planetary Science University of California, Berkeley Berkeley CA USAAbstract Models for the second time‐derivative of the geomagnetic field reveal prominent activity at high latitudes. Alternating patches of positive and negative geomagnetic acceleration propagate to the west at speeds that exceed nominal fluid velocities in the core. We show that waves are a viable interpretation of these observations. Magnetic Rossby waves produce a high‐latitude response with suitable phase velocities. However, the spatial complexity of the prediction is not compatible with the observations. Our preferred interpretation involves zonal MAC waves. These waves can account for the observed geomagnetic field when a stratified layer exists at the top of the core. The required layer has a thickness in excess of 100 km and a buoyancy frequency comparable to the rotation frequency. We anticipate a gradual reduction in the phase velocity over time, leading to a future change in the propagation direction.https://doi.org/10.1029/2021GL094692
spellingShingle Rodrigo Chi‐Durán
Margaret S. Avery
Bruce A. Buffett
Signatures of High‐Latitude Waves in Observations of Geomagnetic Acceleration
Geophysical Research Letters
title Signatures of High‐Latitude Waves in Observations of Geomagnetic Acceleration
title_full Signatures of High‐Latitude Waves in Observations of Geomagnetic Acceleration
title_fullStr Signatures of High‐Latitude Waves in Observations of Geomagnetic Acceleration
title_full_unstemmed Signatures of High‐Latitude Waves in Observations of Geomagnetic Acceleration
title_short Signatures of High‐Latitude Waves in Observations of Geomagnetic Acceleration
title_sort signatures of high latitude waves in observations of geomagnetic acceleration
url https://doi.org/10.1029/2021GL094692
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AT bruceabuffett signaturesofhighlatitudewavesinobservationsofgeomagneticacceleration