Geography Reference
In-Depth Information
The rotation around the 3 axis, we have denoted by
Ω
, the “right ascension of the ascending
node”, while the rotation around the intermediate 1 axis by
i
, the “inclination”.
R
1
(
i
)and
R
3
(
Ω
)
are orthonormal matrices such that (
16.21
)holds.
⎡
⎤
cos
Ω
sin
Ω
0
−
sin
Ω
cos
i
+cos
Ω
cos
i
sin
i
+sin
Ω
sin
i −
cos
Ω
sin
i
cos
i
⎣
⎦
∈
R
3
×
3
.
R
1
(
i
)
R
3
(
Ω
)=
(16.21)
Accordingly, (
16.22
) is a representation of the placement vector
x
in the orthonormal bases
{
e
1
,
e
2
,
e
3
,
O}
and
{
e
1
,
e
2
,
e
3
,
O}
, respectively. Note that (
16.23
)and(
16.24
)hold.
3
3
e
i
x
i
,
e
i
x
i
=
x
=
(16.22)
i
=1
i
=1
x
1
=
x
1
cos
Ω
x
2
sin
Ω
cos
i
+
x
3
sin
Ω
sin
i,
x
2
=
x
1
sin
Ω
+
x
2
cos
Ω
cos
i
−
x
3
cos
Ω
sin
i,
−
(16.23)
x
3
=
x
2
sin
i
+
x
3
cos
i,
x
1
=+
x
1
cos
Ω
+
x
2
sin
Ω
=:
x
,
x
2
=
−x
1
sin
Ω
cos
i
+
x
2
cos
Ω
cos
i
+
x
3
sin
i
=:
y
,
(16.24)
x
3
=+
x
1
sin
Ω
sin
i − x
2
cos
Ω
sin
i
+
x
3
cos
i
=:
z
.
A
1
,A
2
2
O
Corollary 16.1 (Intersection of
E
and
L
).
2
A
1
,A
2
2
O
The intersection of the ellipsoid-of-revolution
E
and the central oblique plane
L
(two-
) is th
e ellipse (
16.25
) of semi-major axis
A
1
=
A
1
dimensional linear manifold thr
ough th
e origin
O
and semi-minor axis
A
2
=
A
1
√
1
E
2
/
√
1
−
−
E
2
cos
2
i
.
1
A
1
,A
2
E
:=
√
1
:=
x
E
2
cos
2
i
,A
1
>A
2
.
A
1
+
y
2
x
2
−
E
2
2
=1
,
A
1
=
A
1
,A
2
=
A
1
∈
R
|
√
1
(16.25)
A
2
−
End of Corollary.
Proof.
[(
x
1
)
2
+(
x
2
)
2
]
A
−
1
+(
16.23
)
⇒
(16.26)
[(
x
1
)
2
+(
x
2
)
2
]
A
−
1
=
A
−
1
[
x
2
+
y
2
cos
2
i
+
z
2
sin
2
i
2
y
z
sin
i
cos
i
]
,
−
[(
x
3
)
2
]
A
−
2
+(
16.23
)
⇒
(16.27)
[(
x
3
)
2
]
A
−
2
=
A
−
2
[
y
2
sin
2
i
+
z
2
cos
2
i
]
,
if
x
=0
,
then
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