Geography Reference
In-Depth Information
distortion Λ 1 ( Δ ) Λ 2 ( Δ ) and the maximal angular shear 2 arcsin[
|
Λ 1 ( Δ )
Λ 2 ( Δ )
|
/ ( Λ 1 ( Δ )+ Λ 2 ( Δ ))]
0 , 30 , 60 , 90 }
as functions of colatitude (polar distance Δ ), namely for Δ given by Δ
∈{
and
six typical polar azimuthal projections.
Tab l e 5 . 2
Distortion data of spherical mappings: “sphere to plane”, azimuthal projections, normal aspect (polar,
direct)
2arcsin | Λ 1 ( Δ ) Λ 2 ( Δ ) |
( Λ 1 ( Δ )+ Λ 2 ( Δ ))
Name
Δ = π/ 2
Φ
Λ 1
Λ 2
Λ 1 Λ 2
(parallel circle)
(meridian)
(area distortion)
(max. ang. distortion)
0
0 00
Equidistant
1.000
1
1.000
30
2 38
(Postel)
1.047
1
1.047
60
10 52
1.209
1
1.209
90
25 39
1.571
1
1.571
0
0
Conformal
1.000
1.000
1.000
30
0
(UPS)
1.072
1.072
1.149
60
0
1.333
1.333
1.778
90
0
2.000
2.000
4.000
0
0 00
Equiareal
1.000
1.000
1.000
30
3 58
1.035
0.966
1.000
60
16 26
1.155
0.866
1.000
90
38 57
1.414
0.707
1.000
0
0 00
Gnomonic
1.000
1.000
1.000
30
8 14
1.155
1.333
1.540
60
38 57
2.000
4.000
8.000
90
180 00
0
0 00
Orthographic
1
1.000
1.000
30
8 14
1
0.866
0.866
60
38 57
1
0.500
0.500
90
180 00
1
0
0
0
0
Lagrange
0.500
0.500
0.250
30
0
conformal
0.536
0.536
0.287
60
0
0.667
0.667
0.445
90
0
1.000
1.000
1.000
In addition, a collection of the distortion energy density tr[C l G l ] / 2=( Λ 1 ( Δ )+ Λ 2 ( Δ )) / 2, the
arithmetic mean of the left principal stretches squared, is presented in Box 5.18 . The distortion
energy density has been given both as a function of colatitude Δ and latitude Φ .Next,bymeans
of Box 5.19 , we outline the computation of the total surface element S of a spherical cap between
a parallel circle of latitude Φ (colatitude Δ )and Φ = π/ 2 (North Pole). Finally, we are prepared
to compute by means of Box 5.20 the distortion energy over a spherical cap, relatively to the six
typical polar azimuthal projections. Note that all integral formulae were taken from Grabner and
Hofreiter ( 1973 ), in particular, 331.10 k (p. 119) 331.11 k (p. 120), and 333.8 b (p. 130).
Box 5.18 (Distortion energy density tr[C l G l ] / 2=( Λ 1 ( Δ )+ Λ 2 ( Δ )) / 2 for various azimuthal
map projections of the sphere, normal aspect (polar aspect)).
Equidistant (Postel):
sin 2 Δ + Δ 2
sin 2 Δ
cos 2 Φ +( 2
Φ ) 2
1
2 ( Λ 1 + Λ 2 )= 1
= 1
2
.
(5.114)
2
cos 2 Φ
 
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