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Table 3 Summation of \(C_{{{\text{site}}1,x}} \left( 0 \right)\), \(C_{{{\text{site}}1,x}} \left( 1 \right)\), \(C_{{{\text{site}}2,x}} \left( 0 \right)\), and \(C_{{{\text{site}}2,x}} \left( 1 \right)\), and the resultant values of \(T_{xx} \left( {1,2} \right)\) and \(T_{xx} \left( {2,1} \right)\)

From: Spatial gradients of geomagnetic temporal variations causing the instability of inter-station transfer functions

Case

\(C_{{{\text{site}}1,x}} \left( 0 \right)\)

\(C_{{{\text{site}}1,x}} \left( 1 \right)\)

\(C_{{{\text{site}}2,x}} \left( 0 \right)\)

\(C_{{{\text{site}}2,x}} \left( 1 \right)\)

\(T_{xx} \left( {1,2} \right)\)

\(T_{xx} \left( {2,1} \right)\)

A

1.00

1.00

1.00

1.00

1.00

1.00

B

1.20

0.80

1.00

1.00

1.00

0.96

C

0.80

1.20

1.30

0.80

0.86

0.96

D

1.00

1.10

1.20

0.80

1.00

0.94