Regional geomagnetic core field and secular variation model over the Iberian Peninsula from 2014 to 2020 based on the R-SCHA technique

Abstract The Earth’s magnetic field originated in the fluid core, the so-called core field, is the dominant contribution to the geomagnetic field. Since ancient times, the core geomagnetic field has been used primarily for geographical orientation and navigation by means of compasses. Nowadays, than...

Full description

Bibliographic Details
Main Authors: Marina Puente-Borque, F. Javier Pavón-Carrasco, Alberto Núñez, José Manuel Tordesillas, Saioa A. Campuzano
Format: Article
Language:English
Published: SpringerOpen 2023-08-01
Series:Earth, Planets and Space
Subjects:
Online Access:https://doi.org/10.1186/s40623-023-01873-w
_version_ 1797577496378474496
author Marina Puente-Borque
F. Javier Pavón-Carrasco
Alberto Núñez
José Manuel Tordesillas
Saioa A. Campuzano
author_facet Marina Puente-Borque
F. Javier Pavón-Carrasco
Alberto Núñez
José Manuel Tordesillas
Saioa A. Campuzano
author_sort Marina Puente-Borque
collection DOAJ
description Abstract The Earth’s magnetic field originated in the fluid core, the so-called core field, is the dominant contribution to the geomagnetic field. Since ancient times, the core geomagnetic field has been used primarily for geographical orientation and navigation by means of compasses. Nowadays, thanks to the large amount of geomagnetic data available, core field models can be developed on a global or regional scale. Global models resolve large-scale geomagnetic field features, while regional models can resolve greater detail over a particular region. The spherical harmonic cap analysis is a widely used technique for regional-scale modelling of the geomagnetic field. In this work we have developed a regional model of the core field and its secular variation between 2014.5 and 2020.5 over the Iberian Peninsula, based on data from Swarm satellites, geomagnetic observatories and repeat stations. Its performance has been validated by comparing the fit to the available geomagnetic data using the regional model and the global models IGRF and CHAOS over the whole spatio-temporal range studied. In order to optimise the model, a detailed study of its input parameters has been carried out, showing that not all parameters have an equal influence on the modelling. This new model reproduces the input data with a root mean square error of 2.9 nT, improving the outcome of global models on this region. The results of this work will allow the Spanish Instituto Geográfico Nacional to produce the magnetic cartography of Iberia and the Balearic Islands in 2020.0, which for the first time will be based on a regional core field model, replacing the polynomial variation method used in the past. Graphical abstract
first_indexed 2024-03-10T22:09:08Z
format Article
id doaj.art-2b8e87800c2541e6a810bb21c973692c
institution Directory Open Access Journal
issn 1880-5981
language English
last_indexed 2024-03-10T22:09:08Z
publishDate 2023-08-01
publisher SpringerOpen
record_format Article
series Earth, Planets and Space
spelling doaj.art-2b8e87800c2541e6a810bb21c973692c2023-11-19T12:39:08ZengSpringerOpenEarth, Planets and Space1880-59812023-08-0175111310.1186/s40623-023-01873-wRegional geomagnetic core field and secular variation model over the Iberian Peninsula from 2014 to 2020 based on the R-SCHA techniqueMarina Puente-Borque0F. Javier Pavón-Carrasco1Alberto Núñez2José Manuel Tordesillas3Saioa A. Campuzano4Facultad de CC. Físicas, Universidad Complutense de MadridFacultad de CC. Físicas, Universidad Complutense de MadridServicio de Geomagnetismo, Instituto Geográfico NacionalServicio de Geomagnetismo, Instituto Geográfico Nacional, Observatorio Geofísico de ToledoFacultad de CC. Físicas, Universidad Complutense de MadridAbstract The Earth’s magnetic field originated in the fluid core, the so-called core field, is the dominant contribution to the geomagnetic field. Since ancient times, the core geomagnetic field has been used primarily for geographical orientation and navigation by means of compasses. Nowadays, thanks to the large amount of geomagnetic data available, core field models can be developed on a global or regional scale. Global models resolve large-scale geomagnetic field features, while regional models can resolve greater detail over a particular region. The spherical harmonic cap analysis is a widely used technique for regional-scale modelling of the geomagnetic field. In this work we have developed a regional model of the core field and its secular variation between 2014.5 and 2020.5 over the Iberian Peninsula, based on data from Swarm satellites, geomagnetic observatories and repeat stations. Its performance has been validated by comparing the fit to the available geomagnetic data using the regional model and the global models IGRF and CHAOS over the whole spatio-temporal range studied. In order to optimise the model, a detailed study of its input parameters has been carried out, showing that not all parameters have an equal influence on the modelling. This new model reproduces the input data with a root mean square error of 2.9 nT, improving the outcome of global models on this region. The results of this work will allow the Spanish Instituto Geográfico Nacional to produce the magnetic cartography of Iberia and the Balearic Islands in 2020.0, which for the first time will be based on a regional core field model, replacing the polynomial variation method used in the past. Graphical abstracthttps://doi.org/10.1186/s40623-023-01873-wGeomagnetismCore fieldSecular variationRegional modellingRevised Spherical Cap Harmonic AnalysisIberia
spellingShingle Marina Puente-Borque
F. Javier Pavón-Carrasco
Alberto Núñez
José Manuel Tordesillas
Saioa A. Campuzano
Regional geomagnetic core field and secular variation model over the Iberian Peninsula from 2014 to 2020 based on the R-SCHA technique
Earth, Planets and Space
Geomagnetism
Core field
Secular variation
Regional modelling
Revised Spherical Cap Harmonic Analysis
Iberia
title Regional geomagnetic core field and secular variation model over the Iberian Peninsula from 2014 to 2020 based on the R-SCHA technique
title_full Regional geomagnetic core field and secular variation model over the Iberian Peninsula from 2014 to 2020 based on the R-SCHA technique
title_fullStr Regional geomagnetic core field and secular variation model over the Iberian Peninsula from 2014 to 2020 based on the R-SCHA technique
title_full_unstemmed Regional geomagnetic core field and secular variation model over the Iberian Peninsula from 2014 to 2020 based on the R-SCHA technique
title_short Regional geomagnetic core field and secular variation model over the Iberian Peninsula from 2014 to 2020 based on the R-SCHA technique
title_sort regional geomagnetic core field and secular variation model over the iberian peninsula from 2014 to 2020 based on the r scha technique
topic Geomagnetism
Core field
Secular variation
Regional modelling
Revised Spherical Cap Harmonic Analysis
Iberia
url https://doi.org/10.1186/s40623-023-01873-w
work_keys_str_mv AT marinapuenteborque regionalgeomagneticcorefieldandsecularvariationmodelovertheiberianpeninsulafrom2014to2020basedontherschatechnique
AT fjavierpavoncarrasco regionalgeomagneticcorefieldandsecularvariationmodelovertheiberianpeninsulafrom2014to2020basedontherschatechnique
AT albertonunez regionalgeomagneticcorefieldandsecularvariationmodelovertheiberianpeninsulafrom2014to2020basedontherschatechnique
AT josemanueltordesillas regionalgeomagneticcorefieldandsecularvariationmodelovertheiberianpeninsulafrom2014to2020basedontherschatechnique
AT saioaacampuzano regionalgeomagneticcorefieldandsecularvariationmodelovertheiberianpeninsulafrom2014to2020basedontherschatechnique