Geography Reference
In-Depth Information
13-21 Sinusoidal Pseudo-Cylindrical Mapping (
Cossin 1570
,
N. Sanson 1675, J. Flamsteed 1646-1719), Compare
with Fig.
13.1
The mapping equations (
13.12
) are derived from (
13.1
) in connection with (
13.8
) and the special
instruction
f
(
Φ
)=
Φ
. The left Jacobi matrix is given by (
13.13
) and the left Cauchy-Green
matrix (G
r
=I
2
)by(
13.14
). The left principal stretches are defined by (
13.15
). The structure of
the coordinate lines are defined by (
13.16
).
x
y
=
R
Λ
cos
Φ
,
(13.12)
Φ
J
l
=
R
cos
Φ
,
−
Λ
sin
Φ
(13.13)
0
1
C
l
=J
l
G
r
J
l
=
R
2
,
cos
2
Φ
−Λ
sin
Φ
cos
Φ
(13.14)
Λ
sin
Φ
cos
ΦΛ
2
sin
2
Φ
+1
−
√
2
2
2+
Λ
2
sin
2
Φ
+
Λ
sin
Φ
4+
Λ
2
sin
2
Φ,
(
Λ
S
)
1
,
2
=
±
(13.15)
√
2
2
2+
Λ
2
sin
2
Φ
Λ
sin
Φ
4+
Λ
2
sin
2
Φ,
(
Λ
S
)
3
,
4
=
±
−
Φ
=
y
R
⇒ x
=
RΛ
cos
y
R
,
(13.16)
x
RΛ
⇒
x
RΛ
.
cos
Φ
=
y
=
R
arccos
13-22 Elliptic Pseudo-Cylindrical Mapping (C. B. Mollweide),
Compare with Fig.
13.2
Starting from the general equation of an ellipse, i.e.
x
2
/a
2
+
y
2
/b
2
= 1, with constant minor axis
b
and major axis
a
=
a
(
Λ
) being a function of spherical longitude, we fix the size of
b
in such a
way that a hemisphere
−
π/
2
≤
Λ
≤
π/
2 is mapped onto a circle of the same area.
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