4.7 Article

Global Evolution and Dynamics of the Geomagnetic Field in the 15-70 kyr Period Based on Selected Paleomagnetic Sediment Records

Journal

JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
Volume 126, Issue 12, Pages -

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1029/2021JB022681

Keywords

geomagnetic field; geomagnetic excursions; paleomagnetic secular variation; Laschamps excursion; paleomagnetic sediment records

Funding

  1. Projekt DEAL

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Reconstructions of the geomagnetic field on long time scales are crucial to understanding the geodynamo processes in the Earth's core. The geomagnetic field exhibits a variety of variations, with different geomagnetic excursions showing distinct features and energy distribution.
Reconstructions of the geomagnetic field on long time scales are important to understand the geodynamo processes in the Earth's core. The geomagnetic field exhibits a range of variations that vary from normal, dipole-dominated secular variation to geomagnetic excursions and reversals. These transitional events are associated with significant directional deviations and very low intensities. Here we present a new, global geomagnetic field model spanning the period 70-15 ka (GGFSS70) that includes three excursions: Norwegian-Greenland Sea, Laschamps, and Mono Lake/Auckland. The model is built from nine globally distributed, high-resolution, well-dated, sedimentary paleomagnetic records. The GGFSS70 indicates that the axial-dipole component changed sign for about 300 years in the middle of the Laschamps excursion (41.25-40.93 ka). The energy comparison at the Earth's surface reveals that the axial-dipole energy is always higher than the non-axial-dipole except over the Laschamps. In the other two excursions, the axial-dipole is reduced by about one order of magnitude for the Norwegian-Greenland Sea excursion and less for the Mono Lake/Auckland. At the core-mantle boundary, the large-scale non-axial-dipole power is comparable to the axial-dipole power, except over the excursions when the axial-dipole decreases, though less clearly for the Mono Lake/Auckland excursion. The axial dipole moment over the 15-70 ka varies from 0 to 8 x 10(22) Am-2, with an average and standard deviation of 5.1 1.5 x 10(22)Am(2). The Laschamps excursion is associated with growth and poleward movement of reversed flux patches and reversed field in the tangent cylinder at the excursion midpoint, which is not the case for the other two excursions.

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