The CHAOS-3 geomagnetic field model and candidates for the 11th generation IGRF
© The Society of Geomagnetism and Earth, Planetary and Space Sciences (SGEPSS); The Seismological Society of Japan; The Volcanological Society of Japan; The Geodetic Society of Japan; The Japanese Society for Planetary Sciences; TERRAPUB 2010
Received: 2 February 2010
Accepted: 1 July 2010
Published: 31 December 2010
As a part of the 11th generation IGRF defined by IAGA, we propose a candidate model for the DGRF 2005, a candidate model for IGRF 2010 and a candidate model for the mean secular variation between 2010 and 2015. These candidate models, the derivation of which is described in the following, are based on the latest model in the CHAOS model series, called “CHAOS-3”. This model is derived from more than 10 years of satellite and ground observatory data. Maximum spherical harmonic degree of the static field is n = 60. The core field time changes are expressed by spherical harmonic expansion coefficients up to n = 20, described by order 6 splines (with 6-month knot spacing) spanning the time interval 1997.0–2010.0. The third time derivative of the squared magnetic field intensity is regularized at the core-mantle boundary. No spatial regularization is applied.
The 11th generation IGRF is based on seven candidate models for DGRF 2005 and for IGRF 2010, and eight candidate models for the mean secular variation (SV) for 2010–2015. These candidate models have been submitted to IAGA working group V-MOD in October 2009 and evaluated by the IGRF task-force group (see paper by Finlay et al., 2010, this issue). In the following, we describe the derivation of three of the submitted candidate models, one for each of the above mentioned model groups. Our three candidates are based on the CHAOS-3 field model (more specific: CHAOS-3α), a new version in the CHAOS model series. Previous versions are CHAOS (Olsen et al., 2006), xCHAOS (Olsen and Mandea, 2008) and CHAOS-2 (Olsen et al., 2009).
Compared to its predecessors, CHAOS-3 is derived from more recent satellite data and using “revised observatory monthly mean values” (which are corrected for external and induced field contributions). In addition, a different regularization scheme is applied to the time changing part of the model.
During the evaluation procedure of the IGRF candidate models it has been found that the degree-1 internal terms of the preliminary model version CHAOS-3α—derived in September 2009 and used as parent model for our IGRF candidate models—for epoch 2010.0 are rather different from those of the other candidate models. This is most probably due to the fact that only data until summer 2009 have been used for model version CHAOS-3α. It is therefore interesting to investigate the effect of including more recent data on the model behavior near 2010.0. The resulting final model, CHAOS-3, allows us to make a further assessment of our model candidates (which are based on CHAOS-3α) and also of the final adopted IGRF model for epoch 2010.0.
For CHAOS-3 we use Ørsted scalar data between March 1999 and December 2009, and vector data between March 1999 and December 2004; CHAMP scalar data between August 2000 and December 2009, and vector data between January 2001 and December 2009; and SAC-C scalar data between January 2001 and December 2004. The same data selection criteria as for the CHAOS-2 model (Olsen et al., 2009) are applied.
a model of the ionospheric (plus induced) field as predicted by the CM4 model (Sabaka et al., 2004), parameterized by the 3-monthly means of F10.7 solar flux, and
a model of the magnetospheric (plus induced) field as predicted by the external field part of CHAOS-2, parameterized by the Est and Ist indices.
A preliminary version of CHAOS-3, named CHAOS-3 α, has been used as parent model for our IGRF candidates. These candidates were derived and submitted at the end of September 2009, when the very recent satellite and observatory data were not yet available. Therefore, this preliminary model (CHAOS-3 α) is based on Ørsted and CHAMP satellite data until August 2009, respectively July 2009, and observatory data until 2009.0. Model parameterization is identical though to that of the final model CHAOS-3, apart from the fact that the extended timespan of the final model leads to slightly more model parameters for describing the time-binned magnetospheric field and the time-varying CHAMP Euler angles, as explained in the following section.
3. Model Parameterization and Regularization
The time dependence of core field coefficients up to spherical harmonic degree n = 20 is described by order 6 B-splines with a 6-month knot separation and five-fold knots at the endpoints, t = 1997.0 and t = 2010.0. This yields 27 interior knots (at 1997.5, 1998.0,…, 2009.5) and 6 exterior knots at each endpoint, 1997.0 and 2010.0, resulting in 31 basic B-spline functions, M l (t). Internal field coefficients for degrees n = 21–60 are static. Time-dependent terms (for degrees n = 1–20) and static terms (for n = 21– 60) together results in a total of 16,920 internal Gauss coefficients.
Large-scale external (magnetospheric) sources are parameterized in a manner similar to the CHAOS-2 model, with an expansion of the remote magnetospheric sources (magnetotail and magnetopause) in Geocentric Solar Magnetospheric (GSM) coordinates (up to n = 2) and of near magnetospheric sources (magnetospheric ring current) in the Solar Magnetic (SM) coordinate system (also up to n = 2). The time dependence of degree-1 magnetospheric terms in SM coordinates is parameterized by the Est and Ist indices (Maus and Weidelt, 2004; Olsen et al., 2005). In addition, we solve for large-scale time-varying degree-1 external coefficients in bins of 12 hours length (for ), or 5 days length (for ), similar as for the CHAOS-2 model. This gives a total of 6,411 external coefficients (6,151 for CHAOS-3 α, due to the slightly shorter time span).
As part of the field modeling we also perform an inflight instrument calibration and solve for the Euler angles of the rotation between the coordinate systems of the vector magnetometer and of the star sensor providing attitude information. For the Ørsted data, this yields two sets of Euler angles, while for CHAMP we solve for Euler angles in bins of 10 days (i.e. 213 sets of angles). This yields additional 3 × (2 + 213) = 639 model parameters (618 for CHAOS-3α). The total number of model parameters is 16,920 + 6,411 + 639 = 23,970 (23,689 for CHAOS-3 α).
Regularization of the third time derivative alone leads to highly oscillating field behavior. To avoid this we also minimize at the core surface at the model endpoints t = 1997.0 and 2010.0. This is implemented via the regularization matrix . Note that only acts on 12 (the first and last six) of the 31 spline basis functions. The parameters λ3 and λ2 control the strength of the regularization. We considered several values for these two parameters and finally selected λ3 = 1 (nT/yr3 )−2 and λ2 = 10 (nT/yr2 )−2.
This regularization is different from that used for CHAOS-2, for which the time average of the second time derivative, , is minimized at the core surface. However, we also derive a model using the same model regularization as CHAOS-2s, but applied to the extended data set of CHAOS-3. In the following sections, this model is referred to as the “extended CHAOS-2s” model.
4. Results and Discussion
Number N of data points, mean, and rms misfit (in nT for the satellite data, and in nT/yr for the observatory data) for CHAOS-3α and CHAOS-3.
Fnonpolar +B B
Fnonpolar + B B
Fnonpolar + B B
The CHAOS-3 rms misfits for the satellite data are slightly lower than those of the CHAOS-3 α model, and lower than those of CHAOS-2 (cf. table 1 of Olsen et al. (2009). Compared to CHAOS-2, most significant is the decrease of the observatory misfit by a factor 2 for the horizontal components and and by about 30% for , which is probably due to the use of revised monthly mean values compared to traditional monthly means. In addition to the lower rms misfit, the non-zero means of the observatory and found in CHAOS-2 are no longer present in CHAOS-3, indicating external field contributions in the traditional monthly means that were used for CHAOS-2. The revised monthly means are obviously less contaminated by external field contributions.
The time change of the sectorial coefficients which represent low-latitude field changes, are better resolved, as indicated by the lower scatter. The temporal variations for the lower degrees are generally well described by the spline models (and especially by CHAOS-3). However, higher degree sectorial terms (e.g., ) show rapid field fluctuations that are less well described by the models because of the applied temporal regularization, which increases with degree n. Obviously small-scale low-latitude rapid fluctuations exist but are not captured by the present spline models.
our candidate model for DGRF-2005 is the degree n = 1–13 part of CHAOS-3 α computed for the epoch t = 2005.0;
our candidate model for IGRF-2010 is the degree n = 1–13 part of CHAOS-3 α computed for the epoch t = 2010.0 (note that 2010 is the last spline knot of this model, but since only data until August 2009 have been used to determine the parent model CHAOS-3 α, an extrapolation in time beyond the data span is performed);
our candidate model for an average secular variation from 2010.0 to 2015.0 is the degree n = 1–8 part of the first time derivative of CHAOS-3 α computed for the epoch t = 2010.0.
Using satellite and observatory data (selected and processed as indicated before), high quality models of the recent geomagnetic field have been developed. They provide a detailed picture of the internal field, of the core field secular variation and secular acceleration at Earth’s surface. Moreover, over the last decade, these models have dramatically improved the core field description at the core-mantle boundary and brought new insights into core dynamics.
Coefficients and data sets for the CHAOS-3 α and CHAOS-3 model versions are available at www.space.dtu.dk/files/magnetic-models/CHAOS-3/.
The Ørsted Project was made possible by extensive support from the Danish Government, NASA, ESA, CNES, DARA and the Thomas B. Thriges Foundation. The support of the CHAMP mission by the German Aerospace Center (DLR) and the Federal Ministry of Education and Research is gratefully acknowledged. We would like to thank the staff of the geomagnetic observatories and INTERMAGNET for supplying high-quality observatory data, and Susan MacMillan for providing us with preliminary observatory hourly mean values for 2009. The work by MM is considered as IPGP contribution 3071.
- Chulliat, A. and K. Telali, World monthly means database project, Publs. Inst. Geophys. Pol. Acad. Sc, C-99(398), 268–274, 2007.Google Scholar
- Finlay, C. C, S. Maus, C. D. Beggan, M. Hamoudi, F. J. Lowes, N. Olsen, and E. Thébault, Evaluation of candidate geomagnetic field models for IGRF-11, Earth Planets Space, 62, this issue, 787–804, 2010.View ArticleGoogle Scholar
- Mandea, M. and N. Olsen, A new approach to directly determine the secular variation from magnetic satellite observations, Geophys. Res. Lett., 33, L15,306, doi:10.1029/2006GL026616, 2006.Google Scholar
- Maus, S. and P. Weidelt, Separating the magnetospheric disturbance magnetic field into external and transient internal contributions using a 1D conductivity model of the Earth, Geophys. Res. Lett., 31, L12,614, doi:10.1029/2004GL020232, 2004.Google Scholar
- Olsen, N., External field contributions in observatory monthly means, Geophys. Res. Abstracts, 11, 2009.Google Scholar
- Olsen, N. and M. Mandea, Investigation of a secular variation impulse using satellite data: The 2003 geomagnetic jerk, Earth Planet. Sci. Lett., 255, 94–105, doi:10.1016/j.epsl.2006.12.008, 2007.View ArticleGoogle Scholar
- Olsen, N. and M. Mandea, Rapidly changing flows in the Earth’s core, Nature Geosci., 1(6), 390, 2008.View ArticleGoogle Scholar
- Olsen, N., T. J. Sabaka, and F. Lowes, New parameterization of external and induced fields in geomagnetic field modeling, and a candidate model for IGRF 2005, Earth Planets Space, 57, 1141–1149, 2005.View ArticleGoogle Scholar
- Olsen, N., H. Lühr, T. J. Sabaka, M. Mandea, M. Rother, L. Tøffner-Clausen, and S. Choi, CHAOS—a model of Earth’s magnetic field derived from CHAMP, Ørsted, and SAC-C magnetic satellite data, Geophys. J. Int., 166,67–75, doi:10.1111/j.1365-246X.2006.02959.x, 2006.View ArticleGoogle Scholar
- Olsen, N., M. Mandea, T. J. Sabaka, and L. Tøffner-Clausen, CHAOS-2—A geomagnetic field model derived from one decade of continuous satellite data, Geophys. J. Int., 179(3), 1477–1487, doi:10.1111/j.1365-246X.2009.04386.x, 2009.View ArticleGoogle Scholar
- Sabaka, T. J., N. Olsen, and M. E. Purucker, Extending comprehensive models of the Earth’s magnetic field with Ørsted and CHAMP data, Geophys. J. Int., 159, 521–547, doi:10.1111/j.1365-246X.2004.02421.x, 2004.View ArticleGoogle Scholar