294 13 “Sphere to cylinder”: pseudo-cylindrical projections
The four roots are then given by (13.6). The postulate of “no area distortion”, i. e.(13.7) now determines the relationship between the unknown functions f and g as (13.8).
(Λ S ) 1,2 = ±
(Λ 2
S ) 1 = ±
√
a + b ,
(Λ S ) 3,4 = ±
(Λ 2
S ) 2 = ±
√
a − b ,
(13.6)
(Λ S ) 1,2 (Λ S ) 3,4 =
=
√
a + b
√
a − b = a
2
− b
2 !
= 1 ,
(13.7)
f
= g
−1
⇔ g = f
−1 .
(13.8)
We therefore end up with the general mapping equations (13.9) and the left principal stretches (13.10).
For the special case f
(Φ) = 1, the left principal stretches can easily calculated as (13.11), which shows
that on the equator, Φ = 0
◦ , we experience isometry (conformality).
x = x(Λ, Φ) = RΛ
cos Φ
f (Φ)
=
R
2 Λ cos Φ
dy
dΦ
,
y = y(Φ) = Rf (Φ) ,
(13.9)
Λ
2
S =
=
1
2f 4 (Λ
2 f
2 sin
2 Φ + f
6 + f
2 + Λ
2 f
2 cos
2 Φ + 2Λ
2 f
f
sin Φ cos Φ)±
±
1
4f 8 (Λ 2 f 2 sin
2 Φ + f 6 + f 2 + Λ 2 f 2 cos 2 Φ + 2Λ 2 f f sin Φ cos Φ) 2 − 1 ,
(13.10)
(Λ S ) 1,2 =
= ±
√
2
2
2 + Λ 2 sin
2 Φ + Λ sin Φ
4 + Λ 2 sin
2 Φ ,
(Λ S ) 3,4 =
= ±
√
2
2
2 + Λ 2 sin
2 Φ − Λ sin Φ
4 + Λ 2 sin
2 Φ .
(13.11)
13-2 Special mapping equations
Special mapping equations for pseudo-cylindrical equal area mappings of the sphere. Sinusoidal pseudocylindrical mapping, elliptic pseudo-cylindrical mapping, parabolic pseudo-cylindrical mapping, rectilinear
pseudo-cylindrical mapping.
The special mapping equations to be considered are the mapping equations of the sinusoidal pseudocylindrical mapping, the elliptic pseudo-cylindrical mapping, the parabolic pseudo-cylindrical mapping, and the rectilinear pseudo-cylindrical mapping. Let us study these special mapping equations in
the sections that follow.
The four roots are then given by (13.6). The postulate of “no area distortion”, i. e.(13.7) now determines the relationship between the unknown functions f and g as (13.8).
(Λ S ) 1,2 = ±
(Λ 2
S ) 1 = ±
√
a + b ,
(Λ S ) 3,4 = ±
(Λ 2
S ) 2 = ±
√
a − b ,
(13.6)
(Λ S ) 1,2 (Λ S ) 3,4 =
=
√
a + b
√
a − b = a
2
− b
2 !
= 1 ,
(13.7)
f
= g
−1
⇔ g = f
−1 .
(13.8)
We therefore end up with the general mapping equations (13.9) and the left principal stretches (13.10).
For the special case f
(Φ) = 1, the left principal stretches can easily calculated as (13.11), which shows
that on the equator, Φ = 0
◦ , we experience isometry (conformality).
x = x(Λ, Φ) = RΛ
cos Φ
f (Φ)
=
R
2 Λ cos Φ
dy
dΦ
,
y = y(Φ) = Rf (Φ) ,
(13.9)
Λ
2
S =
=
1
2f 4 (Λ
2 f
2 sin
2 Φ + f
6 + f
2 + Λ
2 f
2 cos
2 Φ + 2Λ
2 f
f
sin Φ cos Φ)±
±
1
4f 8 (Λ 2 f 2 sin
2 Φ + f 6 + f 2 + Λ 2 f 2 cos 2 Φ + 2Λ 2 f f sin Φ cos Φ) 2 − 1 ,
(13.10)
(Λ S ) 1,2 =
= ±
√
2
2
2 + Λ 2 sin
2 Φ + Λ sin Φ
4 + Λ 2 sin
2 Φ ,
(Λ S ) 3,4 =
= ±
√
2
2
2 + Λ 2 sin
2 Φ − Λ sin Φ
4 + Λ 2 sin
2 Φ .
(13.11)
13-2 Special mapping equations
Special mapping equations for pseudo-cylindrical equal area mappings of the sphere. Sinusoidal pseudocylindrical mapping, elliptic pseudo-cylindrical mapping, parabolic pseudo-cylindrical mapping, rectilinear
pseudo-cylindrical mapping.
The special mapping equations to be considered are the mapping equations of the sinusoidal pseudocylindrical mapping, the elliptic pseudo-cylindrical mapping, the parabolic pseudo-cylindrical mapping, and the rectilinear pseudo-cylindrical mapping. Let us study these special mapping equations in
the sections that follow.
