Geography Reference
In-Depth Information
H 2 ( q ( t ) ,p ( t )) = 1
1
2 ( p 1 + p 2 )
2 ρ 2 (1 + d 02 ( q 2 ) 2 + d 12 q 1 ( q 2 ) 2 +
d 22 ( q 1 ) 2 ( q 2 ) 2 +
(E.95)
+ d 32 ( q 1 ) 3 ( q 2 ) 2 + d 04 ( q 2 ) 4 + d 14 q 1 ( q 2 ) 4 +O λ 2 (( q 1 ) 6 , ( q 2 ) 6 )) .
(iv)Universal Conic Projection (UC) (variant one variant two):
L 2 ( q ( t ) , q ( t )) = 1
2 ( q 1 ) 2 +( q 2 ) 2 +
A 2 cos 2 r 1 (( q 1 ) 2 +( q 2 ) 2 )
2 c 2 n 2 1
e 2 sin 2 r 1 ( q 1 ) 2 +( q 2 ) 2 ×
(E.96)
r 1 ( q 1 ) 2 +( q 2 ) 2
tan 2
π
4
×
2
1+ e sin r 1 ( q 1 ) 2 +( q 2 ) 2
e
−n
e sin r 1 ( q 1 ) 2 +( q 2 ) 2
,
1
A 2 cos 2 r 1 (( q 1 ) 2 +( q 2 ) 2 )
2 c 2 n 2 (1
H 2 ( q ( t ) ,p ( t )) = 1
2 ( p 1 + p 2 )
e 2 sin 2 r 1 ( ( q 1 ) 2 +( q 2 ) 2 )) ×
(E.97)
r 1 ( q 1 ) 2 +( q 2 ) 2
tan 2
π
4
×
2
1+ e sin r 1 ( q 1 ) 2 +( q 2 ) 2
e
−n
e sin r 1 ( q 1 ) 2 +( q 2 ) 2
.
1
2
Box E.6 (The differential equations of a geodesic in
A,B in terms of conformal coordinates
(isometric coordinates) and Maupertuis gauge: Lagrange portrait, two differential equations
of second order, Hamilton portrait, four differential equations of first order).
E
(i)Universal Polar Stereographic Projection (UPS):
A 2
( q 1 )+( q 2 ) 2
q μ +
(1 − e 2 )cos f 1 ( q 1 ) 2 +( q 2 ) 2 sin f 1 ( q 1 ) 2 +( q 2 ) 2
1
×
(E.98)
e 2 sin 2 f 1 ( q 1 ) 2 +( q 2 ) 2 2
 
Search WWH ::




Custom Search