Geography Reference
In-Depth Information
(tan(
Δ/
2))
=
1
2
1
cos
2
(
Δ/
2)
=
1
1+cos
Δ
,
(sin
Δ
)
=cos
Δ,
tan(
Δ/
2)
sin
Δ
1
1+cos
Δ
cos
Δ
=
1
1
lim
Δ→
0
= lim
Δ→
0
2
,
(8.56)
1+
E
1
E/
2
√
1
− E
2
=1
c
2
A
1
Δ→
0
Λ
1
(
Δ
)=
lim
−
E
⇒
E
2
1
E/
2
2
A
1
√
1
E
1+
E
−
c
=
.
−
Parameterized conformal mapping:
α
=
Λ, r
=
f
(
Δ
)
,
1
E/
2
1+
E
cos
Δ
1
B/
2
2
A
1
√
1
− E
2
E
1+
E
−
tan
Δ
f
(
Δ
)=
2
,
−
E
cos
Δ
f
(
Δ
)
→
f
(
Φ
)
,
(8.57)
E
2
1
−
E
E/
2
1+
E
sin
Φ
1
E/
2
tan
π
,
2
A
1
Φ
2
f
(
Φ
)=
√
1
4
−
1+
E
−
E
sin
Φ
−
x
=
r
cos
α
=
f
(
Φ
)cos
Λ, y
=
r
sin
α
=
f
(
Φ
)sin
Λ.
Left principal stretches and left eigenvectors:
Λ
1
=
Λ
2
=
f
(
Φ
)
1
E
2
sin
2
Φ
A
1
cos
Φ
−
,
(8.58)
D
4
X
D
Φ
X
E
Λ
=
(“Easting”)
,
E
Φ
=
=
−
E
Δ
(“Northing”)
,
D
4
X
D
Φ
X
(8.59)
(i)
C
1
Λ
1
=
E
Λ
f
(
Φ
)
1
,
(ii)
C
2
Λ
2
=
E
Φ
f
(
Φ
)
1
E
2
sin
2
Φ
A
1
cos
Φ
E
2
sin
2
Φ
A
1
cos
Φ
−
−
.
Left angular shear:
Σ
l
=
Ψ
l
−
Ψ
r
=0
, Ω
l
=0
.
(8.60)
Parameterized inverse mapping:
f
(
x
)=
1+
x
1
− x
E/
2
=
f
(0) +
1
1!
f
(
x
)
|
x
=0
,
E
cos
Δ
=
x
1
,
(8.61)
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