Geography Reference
In-Depth Information
e
1
0
=
e
S
=+
e
1
sin
φ
0
cos
λ
0
+
e
2
sin
φ
0
sin
λ
0
−
e
3
cos
φ
0
,
e
2
0
=
e
E
=
−
e
1
sin
λ
0
+
e
2
cos
λ
0
,
(3.40)
e
3
0
=
e
V
=+
e
1
cos
φ
0
cos
λ
0
+
e
2
cos
φ
0
sin
λ
0
+
e
3
sin
φ
0
.
{
e
S
,
e
E
,
e
V
|
x
0
}
is a moving frame (repere mobile) at
x
0
:=
x
(
λ
0
,φ
0
,r
):
⎡
⎤
⎡
⎤
⎡
⎤
⎡
⎤
e
1
0
e
2
0
e
3
0
e
S
e
F
e
V
sin
φ
0
cos
λ
0
sin
φ
0
sin
λ
0
−
cos
φ
0
e
1
e
2
e
3
⎣
⎦
=
⎣
⎦
=
⎣
⎦
⎣
⎦
.
sin
λ
0
cos
λ
0
0
cos
φ
0
cos
λ
0
cos
φ
0
sin
λ
0
+sin
φ
0
−
(3.41)
(iv) Parallel transport:
{
e
S
,
e
E
,
e
V
|
x
(
λ
0
,φ
0
,r
)
}
=
{
e
s
,
e
E
,
e
V
|O}
.
(3.42)
Statement:
⎡
⎤
⎡
⎤
⎡
⎤
e
1
0
e
2
0
e
3
0
e
S
e
E
e
V
e
1
e
2
e
3
⎣
⎦
=
⎣
⎦
=R(
λ
0
,φ
0
,r
)
⎣
⎦
,
R(
λ
0
,φ
0
,r
):=R
2
(
π/
2
−
φ
0
)R
3
(
λ
0
)
,
(3.43)
⎡
⎤
⎡
⎤
cos
λ
0
sin
φ
0
0
−
sin
λ
0
cos
λ
0
0
0
sin
φ
0
0
−
cos
φ
0
01 0
cos
φ
0
0 in
φ
0
⎣
⎦
,
R
2
(
π/
2
− φ
0
):=
⎣
⎦
.
R
3
(
λ
0
):=
0
1
S
r
, equatorial as well as meta-equatorial (oblique) frame of reference
Fig. 3.6.
Vertical section of
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