Geography Reference
In-Depth Information
Table 24.4 Residual from a Balanced Least Absolute Value fit (LESS)
No.
ry 1 (m)
ry 2 (m)
ry 3 (m)
1
0.0419930
0.0000000
+0.1886574
2
+0.2921596
0.0000000
0.0788454
3
0.1511354
0.5772763
+0.5135602
4
+0.0000000
+0.2632668
0.2783069
5
+0.4943256
+0.0149275
+0.0000000
6
0.0322810
0.1844494
+0.0000000
7
+0.9364496
+0.0000000
+0.4995037
8
+0.0000000
+0.2710426
+0.0365388
9
+0.6029285
1.2504552
0.1811957
10
0.0381260
+0.0000000
+0.0000000
11
+1.1150286
+0.0000000
0.4470969
12
0.0271904
+0.2160558
+0.1043160
13
0.0595793
0.2013183
0.1691942
14
+0.7286051
+0.4248259
+0.6807238
15
+0.6027258
0.1983727
0.0931333
Table 24.5 Residual from a Minimax fit (MINIMAX)
No.
ry 1 (m)
ry 2 (m)
ry 3 (m)
1
0.6914626
+0.0615821
+0.2846016
2
0.5232632
+0.2105376
+0.2030011
3
0.6914626
0.2812702
+0.6414800
4
0.6914626
+0.6779095
+0.0221739
5
0.0606393
+0.4210982
+0.2376789
6
0.5898076
+0.2813725
+0.2573426
7
+0.3744737
+0.4550569
+0.6914626
8
0.5190582
+0.6914626
+0.2043970
9
+0.1094704
+0.6914626
0.0879036
10
0.6593011
+0.3076530
+0.1412971
11
+0.6914626
+0.6914626
0.6914626
12
0.4712279
+0.5630593
+0.0311289
13
0.6914626
0.1424975
0.2271799
14
+0.3596312
+0.6914626
+0.3268494
15
+0.1433850
0.1146535
0.3755350
number 1 and point number 15 from 834km to 8.34cm. Now as being documented by Tables 24.9
and 24.10 the parameters 7, 8, 9 occur to be significantly large in size compared to the other
parameters.
Because of a priori linearity the ten parameter transformation group C 10 (3) close to the iden-
tity reveals some benefits in practice. Usually three-dimensional Cartesian coordinate transfor-
mations suffer from their necessity to work out iterations due to nonlinearity, a fact which makes
blunder detection by statistical means dicult. Here the assumption of “small” rotation angles
is widely met in practice. Alternatively large orientation parameters could be determined by a
pre-transformation fit. A report of such a procedure will be given elsewhere.
 
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