Geography Reference
In-Depth Information
twenty-one points of the topographic surface of the Earth presented in Table J.1 . Compare with
Fig. J.6 .
Tab l e J . 1
Cartesian coordinates of topographic point (Baltic Sea Level Project)
Station
X (m)
Y (m)
Z (m)
Borkum (Ger)
3,770,667.9989
446,076.4896
5,107,686.2085
Degerby (Fin)
2,994,064.9360
1,112,559.0570
5,502,241.3760
Furuogrund (Swe)
2,527,022.8721
981,957.2890
5,753,940.9920
Hamina (Fin)
2,795,471.2067
1,435,427.7930
5,531,682.2031
Hanko (Fin)
2,959,210.9709
1,254,679.1202
5,490,594.4410
Helgoland (Gcr)
3,706,044.9443
513,713.2151
5,148,193.4472
Helsinki (Fin)
2,885,137.3909
1,342,710.2301
5,509,039.1190
Kemi (Fin)
2,397,071.5771
1,093,330.3129
5,789,108.4470
Klagshamn (Swe)
3,527,585.7675
807,513.8946
5,234,549.7020
Klaipeda (Lit)
3,353,590.2428
1,302,063.0141
5,249,159.4123
List/Sylt (Gcr)
3,625,339.9221
537,853.8704
5,202,539.0255
Molas (Lit)
3,358,793.3811
1,294,907.4149
5,247,584.4010
Mantyluoto (Fin)
2,831,096.7193
1,113,102.7637
5,587,165.0458
Raahe (Fin)
2,494,035.0244
1,131,370.9936
5,740,955.4096
Ratan (Swe)
2,620,087.6160
1,000,008.2649
5,709,322.5771
Spikarna (Swe)
2,828,573.4638
893,623.7288
5,627,447.0693
Stockholm (Swe)
3,101,008.8620
1,013,021.0372
5,462,373.3830
Ustka (Pol)
3,545,014.3300
1,073,939.7720
5,174,949.9470
Vaasa (Fin)
2,691,307.2541
1,063,691.5238
5,664,806.3799
Visby(Swc)
3,249,304.4375
1,073,624.8912
5,364,363.0732
Olands N. U. (Swe)
3,295,551.5710
1,012,564.9063
5,348,113.6687
From the algorithm of Box J.8 , the first polynomial equation of fourth order of the Grobner
basis is obtained as ( J.72 ). Numerical values are provided by Table J.2 .
c 1 x 4 + c 3 x 4 + c 2 x 4 + c 1 x 4 + c 0 =0 ,
c 4 = a 6 b 6 ,c 3 =2 a 6 b 4 +2 a 4 b 6 ,
c 2 = a 6 b 2 +4 a 4 b 4 + a 2 b 6
− a 4 b 2 X 2
− a 4 b 2 Y 2
− a 2 b 4 Z 2 ,
(J.72)
c 1 =2 a 4 b 2 +2 a 2 b 4
2 a 2 b 2 X 2
2 a 2 b 2 Y 2
2 a 2 b 2 Z 2 ,
c 0 = a 2 b 2
b 2 X 2
b 2 Y 2
a 2 Z 2 .
J-3 Gauss Surface Normal Coordinates: Case Study Triaxial Ellipsoid
First, we review surface normal coordinates for the triaxial ellipsoid. Second, it is our duty to
review representative data for the triaxial ellipsoid for the Earth and other celestial bodies.
 
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