Geography Reference
In-Depth Information
Box 8.3 (Equidistant mapping of the ellipsoid-of-revolution to the tangential plane at the
North Pole).
Parameterized mapping:
α
=
Λ, r
=
f
(
Δ
)
,Δ
:=
π/
2
−
Φ,
(8.20)
x
=
r
cos
α
=
f
(
Δ
)cos
Λ, y
=
r
sin
α
=
f
(
Δ
)sin
Λ.
Canonical postulate
Λ
2
=1
,
equidistant mapping of the family of meridians:
Λ
2
=
f
(
Δ
)
(1
−
E
2
cos
2
Δ
)
3
/
2
=1
A
1
(1
− E
2
)
⇔
d
Δ
E
2
)
d
f
=
A
1
(1
−
(8.21)
(1
−
E
2
cos
2
Δ
)
3
/
2
⇒
f
(
Δ
)=
A
1
(1
− E
2
)
Δ
0
d
Δ
E
2
cos
2
Δ
)
3
/
2
.
(1
−
Transformation of surface normal latitude
Φ
to reduced latitude
Φ
∗
:
tan
Φ
∗
=
√
1
−
E
2
tan
Φ
⇔
(8.22)
1
√
1
− E
2
tan
Φ
∗
.
tan
Φ
=
Equidistant mapping of the family of meridians,
elliptic integral of the second kind:
f
(
Δ
)
→ f
(
Φ
)
,
E
2
)
π/
2
π/
2
−Φ
d
Φ
(1
− E
2
sin
2
Φ
)
3
/
2
;
f
(
Φ
)
→ f
(
Φ
∗
)
,
f
(
Φ
∗
)=
A
1
π/
2
π/
2
−Φ
f
(
Φ
)=
A
1
(1
−
1
E
2
cos
2
Φ
∗
d
∗
;
−
(8.23)
f
(
Φ
∗
)
f
(
Δ
∗
)
,
→
f
(
Δ
∗
)=
A
1
Δ
∗
0
1
E
2
sin
2
Δ
d
Δ
=:
A
1
E
(
Δ
∗
,E
)
.
−
Elliptic integral of the second kind:
f
(
Φ
)=
A
1
E
π/
2
−
arc tan
√
1
− E
2
tan
Φ
,E
.
(8.24)
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