Geography Reference
In-Depth Information
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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