Changes in Earth's core-generated magnetic field, as observed by Swarm

Research output: Contribution to conferenceConference abstract for conferenceResearchpeer-review

Abstract

By far the largest part of the Earth's magnetic field is generated by motions taking place within our planet's liquid metal outer core. Variations of this core-generated field thus provide us with a unique means of probing the dynamics taking place in the deepest reaches of the Earth. In this contribution, we will present the core-generated magnetic field, and its recent time changes, as seen by ESA's Earth explorer mission Swarm.
We will present a new time-dependent geomagnetic field model, called CHAOS-6, derived from satellite data collected by the Swarm constellation, as well as data from the previous missions CHAMP and Oersted together with ground observatory data. Advantage is taken of the constellation aspect of the Swarm mission by ingesting field differences along track and across track between the lower pair of Swarm satellites. Evaluating the global field model at the outer boundary of the source region, the core-mantle boundary, we present maps of the detailed structure of the geodynamo, and how this is presently evolving. Both the trend (secular variation) and accelerations in the field changes since the launch of the Swarm mission will be presented.
Assuming that field changes are primarily a result of advective processes, thanks to the high electrical conductivity of the core, and that the responsible core flows are essentially columnar, due to the organizing influence of the Coriolis force, we derive maps of the underlying core flow. The structure of this core flow, its changes over recent years, and implications for our understanding of the geodynamo process will be discussed.
Original languageEnglish
Publication date2016
Number of pages1
Publication statusPublished - 2016
EventESA Living Planet Symposium 2016 - Prague, Czech Republic
Duration: 9 May 201613 May 2016
http://lps16.esa.int/

Conference

ConferenceESA Living Planet Symposium 2016
CountryCzech Republic
CityPrague
Period09/05/201613/05/2016
Internet address

Cite this

Finlay, C., Olsen, N., Gillet, N., Kotsiaros, S., Tøffner-Clausen, L., & Hammer, M. D. (2016). Changes in Earth's core-generated magnetic field, as observed by Swarm. Abstract from ESA Living Planet Symposium 2016, Prague, Czech Republic.
Finlay, Chris ; Olsen, Nils ; Gillet, Nicolas ; Kotsiaros, Stavros ; Tøffner-Clausen, Lars ; Hammer, Magnus Danel. / Changes in Earth's core-generated magnetic field, as observed by Swarm. Abstract from ESA Living Planet Symposium 2016, Prague, Czech Republic.1 p.
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Finlay, C, Olsen, N, Gillet, N, Kotsiaros, S, Tøffner-Clausen, L & Hammer, MD 2016, 'Changes in Earth's core-generated magnetic field, as observed by Swarm', ESA Living Planet Symposium 2016, Prague, Czech Republic, 09/05/2016 - 13/05/2016.

Changes in Earth's core-generated magnetic field, as observed by Swarm. / Finlay, Chris; Olsen, Nils; Gillet, Nicolas ; Kotsiaros, Stavros; Tøffner-Clausen, Lars; Hammer, Magnus Danel.

2016. Abstract from ESA Living Planet Symposium 2016, Prague, Czech Republic.

Research output: Contribution to conferenceConference abstract for conferenceResearchpeer-review

TY - ABST

T1 - Changes in Earth's core-generated magnetic field, as observed by Swarm

AU - Finlay, Chris

AU - Olsen, Nils

AU - Gillet, Nicolas

AU - Kotsiaros, Stavros

AU - Tøffner-Clausen, Lars

AU - Hammer, Magnus Danel

PY - 2016

Y1 - 2016

N2 - By far the largest part of the Earth's magnetic field is generated by motions taking place within our planet's liquid metal outer core. Variations of this core-generated field thus provide us with a unique means of probing the dynamics taking place in the deepest reaches of the Earth. In this contribution, we will present the core-generated magnetic field, and its recent time changes, as seen by ESA's Earth explorer mission Swarm. We will present a new time-dependent geomagnetic field model, called CHAOS-6, derived from satellite data collected by the Swarm constellation, as well as data from the previous missions CHAMP and Oersted together with ground observatory data. Advantage is taken of the constellation aspect of the Swarm mission by ingesting field differences along track and across track between the lower pair of Swarm satellites. Evaluating the global field model at the outer boundary of the source region, the core-mantle boundary, we present maps of the detailed structure of the geodynamo, and how this is presently evolving. Both the trend (secular variation) and accelerations in the field changes since the launch of the Swarm mission will be presented. Assuming that field changes are primarily a result of advective processes, thanks to the high electrical conductivity of the core, and that the responsible core flows are essentially columnar, due to the organizing influence of the Coriolis force, we derive maps of the underlying core flow. The structure of this core flow, its changes over recent years, and implications for our understanding of the geodynamo process will be discussed.

AB - By far the largest part of the Earth's magnetic field is generated by motions taking place within our planet's liquid metal outer core. Variations of this core-generated field thus provide us with a unique means of probing the dynamics taking place in the deepest reaches of the Earth. In this contribution, we will present the core-generated magnetic field, and its recent time changes, as seen by ESA's Earth explorer mission Swarm. We will present a new time-dependent geomagnetic field model, called CHAOS-6, derived from satellite data collected by the Swarm constellation, as well as data from the previous missions CHAMP and Oersted together with ground observatory data. Advantage is taken of the constellation aspect of the Swarm mission by ingesting field differences along track and across track between the lower pair of Swarm satellites. Evaluating the global field model at the outer boundary of the source region, the core-mantle boundary, we present maps of the detailed structure of the geodynamo, and how this is presently evolving. Both the trend (secular variation) and accelerations in the field changes since the launch of the Swarm mission will be presented. Assuming that field changes are primarily a result of advective processes, thanks to the high electrical conductivity of the core, and that the responsible core flows are essentially columnar, due to the organizing influence of the Coriolis force, we derive maps of the underlying core flow. The structure of this core flow, its changes over recent years, and implications for our understanding of the geodynamo process will be discussed.

M3 - Conference abstract for conference

ER -

Finlay C, Olsen N, Gillet N, Kotsiaros S, Tøffner-Clausen L, Hammer MD. Changes in Earth's core-generated magnetic field, as observed by Swarm. 2016. Abstract from ESA Living Planet Symposium 2016, Prague, Czech Republic.