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Table 3 DOvCs of T zz , T xx , T yy , T xy , T xz and T yz for n = 200 and m = 2.

From: Optimal combination of integral solutions of gradiometric boundary value problem using variance component estimation in Earth gravitational modelling

 

5.74 × 10−9

1.6 × 10−6

5.64 × 10−9

1.57 × 10−6

5.64 × 10−9

1.57 × 10−6

7.00 × 10−7

1.96 × 10−4

5.72 × 10−9

1.60 × 10−6

9.60 × 10−6

2.7 × 10−4