TY - JOUR
T1 - Improving total field geomagnetic secular variation modeling from a new set of cross-over marine data
AU - Pavón-Carrasco, F. Javier
AU - Torta, J. Miquel
AU - Catalán, Manuel
AU - Talarn, àngela
AU - Ishihara, Takemi
N1 - Funding Information:
This study was funded by the grant 2009 SGR 507 of Generalitat de Catalunya , and the projects CTM2010-21312-C03-01, and CGL2011-24790 of the Spanish Ministerio de Economía y Competitividad. F.J.P-C. acknowledges the ME/Fulbright postdoctoral contract CT-2010-0663. The authors are grateful to Ingo Wardinski and an anonymous referee for their useful comments which helped to improve the manuscript. Gregg McIntosh is also acknowledged for his careful review of the entire manuscript.
PY - 2013/3
Y1 - 2013/3
N2 - A new set of cross-over marine data has been used to generate a regional model for the secular variation of the total geomagnetic field, showing the potential of the suggested approach for gaining a better knowledge of the field over oceanic regions. The model, which is valid for the Northern Atlantic region during the temporal interval 1960-2000, was obtained using spherical cap harmonic analysis (SCHA) in space and penalized splines in time. The maximum spatial expansion is equivalent to degree 9 in ordinary spherical harmonic analysis. Annual mean intensity data from different geomagnetic observatories have been used to improve the spatial and temporal resolution of the original dataset. Results indicate that the regional model improves, in terms of the root mean square error, the prediction given by the 11th generation of IGRF and CM4 global models, especially for the geomagnetic observatories considered. We also provide the uncertainty of the model coefficients and the secular variation prediction given by a bootstrap algorithm. The model is available in the EarthRef. org Digital Archive at http://earthref.org/ERDA/1728/.
AB - A new set of cross-over marine data has been used to generate a regional model for the secular variation of the total geomagnetic field, showing the potential of the suggested approach for gaining a better knowledge of the field over oceanic regions. The model, which is valid for the Northern Atlantic region during the temporal interval 1960-2000, was obtained using spherical cap harmonic analysis (SCHA) in space and penalized splines in time. The maximum spatial expansion is equivalent to degree 9 in ordinary spherical harmonic analysis. Annual mean intensity data from different geomagnetic observatories have been used to improve the spatial and temporal resolution of the original dataset. Results indicate that the regional model improves, in terms of the root mean square error, the prediction given by the 11th generation of IGRF and CM4 global models, especially for the geomagnetic observatories considered. We also provide the uncertainty of the model coefficients and the secular variation prediction given by a bootstrap algorithm. The model is available in the EarthRef. org Digital Archive at http://earthref.org/ERDA/1728/.
KW - Geomagnetic marine data
KW - Geomagnetism
KW - North Atlantic Ocean
KW - Regional modeling
KW - Secular variation
KW - Spherical cap harmonic analysis
UR - http://www.scopus.com/inward/record.url?scp=84873127260&partnerID=8YFLogxK
U2 - 10.1016/j.pepi.2013.01.002
DO - 10.1016/j.pepi.2013.01.002
M3 - Article
AN - SCOPUS:84873127260
SN - 0031-9201
VL - 216
SP - 21
EP - 31
JO - Physics of the Earth and Planetary Interiors
JF - Physics of the Earth and Planetary Interiors
ER -