Geography Reference
In-Depth Information
C l =J l G r J l =
π 2
,
4cos 2 t
= 2 R 2
πΛ tan t cos Φ
−πΛ tan t cos Φ π 2 cos 2 Φ ( π 2 +4 Λ 2 tan 2 t )
16 cos 2 t
(13.24)
det(C l − Λ S G l )=
= R 2
8
2
π 2 cos 2 t − Λ S cos 2 Φ
π Λ tan t cos Φ
2cos 2 t Λ 2 tan 2 t + π 4
=
(13.25)
cos 2 Φ
2
π Λ tan t cos Φ
− Λ S
=0 .
13-23 Parabolic Pseudo-Cylindrical Mapping (J. E. E. Craster),
Compare with Fig. 13.3
This mapping is defined in such a way that the meridians except the central meridian, which is a
straight line, are equally spaced parabolas. Parallels are unequally spaced straight lines, farthest
apart near the equator. The mapping equations are defined by ( 13.26 ). The left Jacobi matrix is
given by ( 13.27 ) and the left Cauchy-Green matrix is given by ( 13.28 )(G r =I 2 ). As can be seen
from Fig. 13.3 , map distortion is severe near outer meridians at high latitudes.
x =
= 3
π 2cos 2 Φ
3 1 ,
(13.26)
y =
= 3 πR sin Φ
3 ,
J l =
= R 3
π
2cos 2 3
,
4
3 Λ sin 2 3
1
(13.27)
π
3 cos 3
0
C l =J l G r J l =
.
2cos 2 3
12 Λ sin 2 3 1 2cos 2 3 16 Λ 2 sin 2 2 3 + π 2 cos 2 3
9 1
2cos 2 3 2
12 Λ sin 2 3 1
= R 2
3 π
(13.28)
 
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