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Table 5 Number N, Huber-weighted mean, and standard deviation \(\sigma\) computed from the residuals of the satellite data for each vector component and split into polar (poleward \(\pm 55^{\circ }\)) and non-polar (equatorward \(\pm 55^{\circ }\)) QD latitudes. Note that non-polar scalar data were not used in the model parameter estimation—statistics are only shown for completeness

From: Co-estimating geomagnetic field and calibration parameters: modeling Earth’s magnetic field with platform magnetometer data

Dataset

Quasi-dipole latitude

Component

N

mean (nT)

\(\sigma\) (nT)

CHAMP

Non-polar

\(B_r\)

707131

0.02

1.93

\(B_\theta\)

707131

− 0.11

2.84

\(B_\phi\)

707131

0.03

2.32

F

707131

0.01

1.93

Polar

F

200084

− 0.02

5.10

CryoSat-2 FGM1

Non-polar

\(B_r\)

958362

− 0.06

4.39

\(B_\theta\)

958362

− 0.31

5.76

\(B_\phi\)

958362

0.06

6.49

F

958362

0.06

4.18

Polar

F

331097

− 0.28

7.56

CryoSat-2 FGM2

Non-polar

\(B_r\)

958362

− 0.03

6.42

\(B_\theta\)

958362

− 0.29

6.01

\(B_\phi\)

958362

0.07

6.55

F

958362

0.18

4.86

Polar

F

331097

− 1.70

8.21

CryoSat-2 FGM3

Non-polar

\(B_r\)

958362

− 0.07

4.76

\(B_\theta\)

958362

− 0.23

5.71

\(B_\phi\)

958362

0.04

6.80

F

958362

0.12

4.35

Polar

F

331097

− 1.01

7.86

GRACE-A

Non-polar

\(B_r\)

1082071

− 0.12

11.40

\(B_\theta\)

1082071

− 0.24

10.48

\(B_\phi\)

1082071

− 0.79

13.57

F

1082071

− 0.16

10.59

Polar

F

356988

0.32

15.56

GRACE-B

Non-polar

\(B_r\)

997802

− 0.30

11.77

\(B_\theta\)

997802

− 0.69

11.09

\(B_\phi\)

997802

− 0.68

12.35

F

997802

0.02

11.53

Polar

F

331516

− 0.24

15.56

Swarm-A

Non-polar

\(B_r\)

817400

− 0.03

1.65

\(B_\theta\)

817400

− 0.06

2.97

\(B_\phi\)

817400

− 0.02

2.59

F

817400

− 0.03

2.06

Polar

F

218776

0.22

4.66

Swarm-B

Non-polar

\(B_r\)

809720

− 0.09

1.63

\(B_\theta\)

809720

− 0.05

3.02

\(B_\phi\)

809720

− 0.04

2.61

F

809720

− 0.01

2.03

Polar

F

218106

0.30

4.29