Geography Reference
In-Depth Information
Tab l e I . 2
Airy optimal dilatation factor
ρ
0
for a symmetric strip, generalized UPC, WGS 84. Symmetric strip
[
Λ
W
=
Λ
0
−
ΔΦ, Φ
0
+
ΔΦ
=
Φ
N
], strip width 3
◦
,
ΔΦ
=1
.
5
◦
ΔΛ, Λ
0
+
ΔΛ
=
Λ
E
]
×
[
Φ
S
=
Φ
0
−
Zone
Φ
0
Φ
S
Φ
N
ρ
0
Zone
Φ
0
Φ
S
Φ
N
ρ
0
0
0
◦
−
1
.
5
◦
+1
.
5
◦
0.999887
±
1
±
3
◦
±
1
.
5
◦
±
4
.
5
◦
0.999886
±
2
±
6
◦
±
4
.
5
◦
±
7
.
5
◦
0.999884
±
3
±
9
◦
±
7
.
5
◦
±
10
.
5
◦
0.999881
12
◦
10
.
5
◦
13
.
5
◦
15
◦
13
.
5
◦
16
.
5
◦
±
4
±
±
±
0.999876
±
5
±
±
±
0.999870
18
◦
16
.
5
◦
19
.
5
◦
21
◦
19
.
5
◦
22
.
5
◦
±
6
±
±
±
0.999862
±
7
±
±
±
0.999852
24
◦
22
.
5
◦
25
.
5
◦
27
◦
25
.
5
◦
28
.
5
◦
±
8
±
±
±
0.999840
±
9
±
±
±
0.999826
30
◦
28
.
5
◦
31
.
5
◦
33
◦
31
.
5
◦
34
.
5
◦
±
10
±
±
±
0.999809
±
11
±
±
±
0.999789
36
◦
34
.
5
◦
37
.
5
◦
39
◦
37
.
5
◦
40
.
5
◦
±
12
±
±
±
0.999764
±
13
±
±
±
0.999735
42
◦
40
.
5
◦
43
.
5
◦
45
◦
43
.
5
◦
46
.
5
◦
±
14
±
±
±
0.999699
±
15
±
±
±
0.999656
48
◦
46
.
5
◦
49
.
5
◦
51
◦
49
.
5
◦
52
.
5
◦
±
16
±
±
±
0.999602
±
17
±
±
±
0.999535
54
◦
52
.
5
◦
55
.
5
◦
57
◦
55
.
5
◦
58
.
5
◦
±
18
±
±
±
0.999450
±
19
±
±
±
0.999341
60
◦
58
.
5
◦
61
.
5
◦
63
◦
61
.
5
◦
64
.
5
◦
±
20
±
±
±
0.999197
±
21
±
±
±
0.999002
66
◦
64
.
5
◦
67
.
5
◦
69
◦
67
.
5
◦
70
.
5
◦
±
22
±
±
±
0.998729
±
23
±
±
±
0.998330
72
◦
70
.
5
◦
73
.
5
◦
75
◦
73
.
5
◦
76
.
5
◦
±
24
±
±
±
0.997714
±
25
±
±
±
0.996691
78
◦
76
.
5
◦
79
.
5
◦
81
◦
79
.
5
◦
82
.
5
◦
±
26
±
±
±
0.994804
±
27
±
±
±
0.990705
84
◦
82
.
5
◦
85
.
5
◦
87
◦
85
.
5
◦
88
.
5
◦
±
28
±
±
±
0.978842
±
29
±
±
±
0.910273
Tab l e I . 3
Airy optimal dilatation factor
ρ
0
for a symmetric strip, generalized UPC, WGS 84. Symmetric strip
[
Λ
W
=
Λ
0
−
ΔΦ, Φ
0
+
ΔΦ
=
Φ
N
], strip width 6
◦
,
ΔΦ
=3
◦
ΔΛ, Λ
0
+
ΔΛ
=
Λ
E
]
×
[
Φ
S
=
Φ
0
−
Zone
Φ
0
Φ
S
Φ
N
ρ
0
Zone
Φ
0
Φ
S
Φ
N
ρ
0
0
◦
3
◦
+3
◦
6
◦
3
◦
9
◦
0
−
0.999546
±
1
±
±
±
0.999536
±
±
12
◦
±
9
◦
±
15
◦
±
±
18
◦
±
15
◦
±
21
◦
2
0.999504
3
0.999448
±
±
24
◦
±
21
◦
±
27
◦
±
±
30
◦
±
27
◦
±
33
◦
4
0.999362
5
0.999236
±
36
◦
±
33
◦
±
39
◦
±
42
◦
±
39
◦
±
45
◦
±
6
0.999057
±
7
0.998796
±
48
◦
±
45
◦
±
51
◦
±
54
◦
±
51
◦
±
57
◦
±
8
0.998407
±
9
0.997799
±
60
◦
±
57
◦
±
63
◦
±
66
◦
±
63
◦
±
69
◦
±
10
0.996782
±
11
0.994899
72
◦
69
◦
75
◦
78
◦
75
◦
81
◦
±
12
±
±
±
0.990804
±
13
±
±
±
0.978942
84
◦
81
◦
87
◦
±
14
±
±
±
0.910374
Example I.3 ([95
◦
<Λ<
145
◦
]
×
[
−
12
◦
<Φ<
+8
◦
]).
For the Airy optimal UPC, we have chosen a strip width of 6
◦
between
Φ
S
=
12
◦
and
Φ
N
=8
◦
of
southern and northern latitude, in particular, to match the geographic region of Indonesia. Once
we refer to WGS 84, the strip system as well as the dilatation factor
ρ
0
per strip is illustrated by
Fig.
I.3
, namely for the zones 0
,
−
±
,
−
2.
End of Example.
Furthermore, we computed by means of (
I.34
) the left principal stretches
Λ
1
=
Λ
2
=
Λ
S
(
Φ
0
,Φ
;
ρ
0
)
of each
st
rip and plotted them in Figs.
I.4
,
I.5
,and
I.6
. Moreover, Tables
I.4
and
I.5
give the
latitu
de
Φ
of each strip according to the strip width
ρ
0
and
Φ
0
along which the mapping is equidis-
tant.
Φ
is determined by solving (
I.34
) for given strip width,
ρ
0
and
Φ
0
under the condition that
Λ
1
=
Λ
2
= 1 holds. Obviously, the variation of the left principal stretch
Λ
1
=
Λ
2
=
Λ
S
(
Φ
0
,Φ
;
ρ
0
)
is small within the chosen strip. Alternatively, we may say that the radius of the left Tissot circle
Λ
1
=
Λ
2
=
Λ
S
(
Φ
0
,Φ
:
ρ
0
) varies only for a small amount, a favourable result of the Airy optimal
UPC.
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