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Table 1 Performance of the degree 360 Slepian joint satellite and near-surface magnetic anomaly model (S360)

From: Utility of Slepian basis functions for modeling near-surface and satellite magnetic anomalies of the Australian lithosphere

Data

Input (nT)

S360 estimates (nT)

CC

RMS errors

Max.; Min.

Avg.

Std.

Max.; Min.

Avg.

Std.

CHAMP satellite vector components

 B r

25.66; −19.23

(25.66; −17.51)

0.45

(1.56)

5.26

(5.96)

24.31; −20.74

(24.31; −18.74)

0.39

(1.44)

5.04

(5.77)

0.95

(0.98)

1.57

(1.28)

 B θ

23.03; −16.83

(12.98; −9.84)

0.79

(0.57)

4.31

(4.69)

22.18; −17.60

(16.89; −17.60)

0.17

(−0.17)

3.96

(4.41)

0.91

(0.94)

1.88

(1.77)

 B φ

12.98; −11.25

(12.98; −9.84)

0.23

(0.26)

3.37

(3.67)

11.29; −9.86

(10.97; −8.75)

0.12

(0.14)

2.99

(3.38)

0.90

(0.92)

1.47

(1.41)

Near-surface total intensities

 ΔT

749.8; −509.2

(749.8; −509.2)

−2.55

(7.82)

102.9

(116.1)

832.4; −455.0

(832.4; −455.0)

−1.99

(3.93)

95.8

(113.6)

0.93

(0.97)

38.1

(28.5)

  1. Statistics include the amplitude maximum (Max.), minimum (Min.), average (Avg.), and standard deviation (Std.) values, and the related correlation coefficients (CC) and root-mean-squared (RMS) errors of the input and estimated anomaly data. The numbers in parentheses are for the Australian mainland and Tasmania