The BGS magnetic field candidate models for the 10th generation IGRF

被引:13
作者
Lesur, V [1 ]
Macmillan, S [1 ]
Thomson, A [1 ]
机构
[1] British Geol Survey, Edinburgh EH9 3LA, Midlothian, Scotland
来源
EARTH PLANETS AND SPACE | 2005年 / 57卷 / 12期
关键词
IGRF; geomagnetic field; geomagnetic secular variation;
D O I
10.1186/BF03351899
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
In this paper we describe the derivation of the BGS candidate models for the 10th generation International Geomagnetic Reference Field. Our data set comprised quiet night-time data from the Orsted and Champ satellites spanning 1999.2-2004.6 and observatory hourly means spanning 1999.0-2004.0. To improve the secular variation estimates for 2005.0-2010.0 predictions based on application of linear prediction filters to long series of observatory annual means were also used. These data were fitted by a spherical harmonic "parent" model with an internal field of maximum degree 36, a quadratic dependence on time up to degree 8, a linear dependence on time up to degree 12, an external field of maximum degree 2 with linear dependence on time, annual and semi-annual variations, and Dst dependence for degree 1 terms. Additionally for the external field, non-zonal degree 1 coefficients in the Geocentric Equatorial Inertial reference frame with annual variations and dependence on the Interplanetary Magnetic Field Y-component are included. The candidate models were then based, for the main field, on an extrapolation to 2005.0 of the truncated parent model, and for the secular variation, on its extrapolation to 2007.5. This latter set of coefficients was then used to generate a synthetic data set at the Earth's surface and this set was augmented with long term linear predictions of observatory annual means, to produce the final candidate secular variation model at 2007.5.
引用
收藏
页码:1157 / 1163
页数:7
相关论文
共 10 条
[1]   SPACE PHYSICS COORDINATE TRANSFORMATIONS - A USER GUIDE [J].
HAPGOOD, MA .
PLANETARY AND SPACE SCIENCE, 1992, 40 (05) :711-717
[2]   Modelling of attitude error in vector magnetic data: application to Orsted data [J].
Holme, R .
EARTH PLANETS AND SPACE, 2000, 52 (12) :1187-1197
[3]   LARGE-SCALE, NEAR-FIELD MAGNETIC-FIELDS FROM EXTERNAL SOURCES AND THE CORRESPONDING INDUCED INTERNAL FIELD [J].
LANGEL, RA ;
ESTES, RH .
JOURNAL OF GEOPHYSICAL RESEARCH, 1985, 90 (NB3) :2487-2494
[4]  
Lesur V, 2005, GEOPHYS J INT, V160, P79, DOI 10.1111/j.1365-246X.2004.02479.X
[5]   A more realistic estimate of the variances and systematic errors in spherical harmonic geomagnetic field models [J].
Lowes, FJ ;
Olsen, N .
GEOPHYSICAL JOURNAL INTERNATIONAL, 2004, 157 (03) :1027-1044
[6]   The 2000 revision of the joint UK/US geomagnetic field models and an IGRF 2000 candidate model [J].
Macmillan, S ;
Quinn, JM .
EARTH PLANETS AND SPACE, 2000, 52 (12) :1149-1162
[7]   Separating the magnetospheric disturbance magnetic field into external and transient internal contributions using a 1D conductivity model of the Earth [J].
Maus, S ;
Weidelt, P .
GEOPHYSICAL RESEARCH LETTERS, 2004, 31 (12) :L126141-4
[8]  
McLean S., 2004, US UK WORLD MAGNETIC
[9]   A model of the geomagnetic field and its secular variation for epoch 2000 estimated from Orsted data [J].
Olsen, N .
GEOPHYSICAL JOURNAL INTERNATIONAL, 2002, 149 (02) :454-462
[10]   A comprehensive model of the quiet-time, near-Earth magnetic field: phase 3 [J].
Sabaka, TJ ;
Olsen, N ;
Langel, RA .
GEOPHYSICAL JOURNAL INTERNATIONAL, 2002, 151 (01) :32-68