Geography Reference
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Fig. 16.3. Oblique reference frame
{
e 1 , e 2 , e 3 ,
O}
with respect to the normal reference frame
{
e 1 , e 2 , e 3 ,
O}
[( x 1 ) 2 +( x 2 ) 2 ] A 2
1
+( x 3 ) 2 A 2
2
E 2 A 1 ,A 2 :=
R 3 |
=1 ,A 1 R + ,A 2 R + }
along the principal axes of
{
x
A 1 + cos 2 i
y =1 ,
[( x 1 ) 2 +( x 2 ) 2 ] A 1 +[( x 3 ) 2 ] A 2 = x 2
+ sin 2 i
A 2
A 1
A 2 = A 1 (1
E 2 )
(16.28)
x 2
A 1 +
y 2
A 1 (1
E 2 ) [(1 − E 2 )cos 2 i +sin 2 i ]= x 2
y 2
A 1 (1
E 2 ) (1 − E 2 cos 2 i )=1 .
A 1 +
End of Proof.
In the plane {x ,y }∈{ x R
2
|Ax + By + C =0 } , we introduce circle-reduced meta-longitude
α in order to parameterize
E
A 1 ,A 2 , ,namelyby( 16.29 ), illustrated by Fig. 16.4 .
x = A 1 cos α = A 1 sin α , α = π
1
2
α,
(16.29)
y = A 2 sin α = A 2 cos α , α = π
α .
2
In terms of circle-reduced metalongitude α or of circular reduced meta-pole distance α = π/ 2 −α ,
we are able to represent the arc length of E
1
A 1 ,A 2 , as an elliptic integral of the second kind.
Corollary 16.2 (Arc length of E
1
A 1 ,A 2
).
1
A 1
The arc length s ( α )of
can be represented by ( 16.30 ) with respect to the elliptic integral
of the second kind E ( · ; E ) and the first relative eccentricity E := (1 − A 2 /A 1 ) 1 / 2 .Aseries
expansion of s ( α )uptoorder E 1 / 2 is provided by ( 16.31 ).
E
,A 2
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