Geography Reference
In-Depth Information
Proof (equiareal cylindrical mapping).
Next, we deal with the mapping equations of equiareal type constrained to the equidistance postu-
late on two parallel circles. Again, we enjoy the condition of an equiareal mapping of type (
10.28
).
x
y
=
R
Λ
cos
Φ
0
,
(10.27)
sin
Φ/
cos
Φ
0
Λ
1
=1
/Λ
2
=cos
Φ
0
/
cos
Φ,
(10.28)
Λ
2
=1
/Λ
1
=cos
Φ/
cos
Φ
0
.
Starting from the above relations, we obtain
(
Λ
1
1)
2
+(
Λ
2
1)
2
−
−
=
2
=
(cos
Φ
0
/
cos
Φ
−
1)
2
+(cos
Φ/
cos
Φ
0
−
1)
2
2
=
(10.29)
cos
4
Φ
0
−
2cos
Φ
cos
3
Φ
0
+2cos
2
Φ
cos
2
Φ
0
−
2cos
3
Φ
cos
Φ
0
+cos
4
Φ
=
1
2
,
cos
2
Φ
0
cos
2
Φ
Φ
1
2sin
Φ
1
cos
Φ
∗
cos
2
Φ
0
×
d
Φ
∗
I
A
(equiareal) =
0
(10.30)
(cos
4
Φ
0
−
2cos
Φ
∗
cos
3
Φ
0
+2cos
2
Φ
∗
cos
2
Φ
0
−
2cos
3
Φ
∗
cos
Φ
0
+cos
4
Φ
∗
)
.
×
Auxillary integrals:
d
Φ
∗
cos
Φ
∗
=lntan
π
=
1
4
+
Φ
∗
2
ln
1+cos
Φ
∗
cos
Φ
∗
,
(10.31)
2
1
−
d
Φ
∗
=
Φ
∗
,
d
Φ
∗
cos
2
Φ
∗
=
Φ
∗
2
+
sin 2
Φ
∗
4
=
Φ
∗
2
+
1
2
sin
Φ
∗
cos
Φ
∗
,
(10.32)
d
Φ
∗
cos
Φ
∗
=sin
Φ
∗
,
d
Φ
∗
cos
3
Φ
∗
=
1
3
sin
Φ
∗
(2 + cos
2
Φ
∗
)
.
For the unknown parameter
Φ
0
, we shall compute the Airy distortion energy for the given region
of
Φ
=
±
85
◦
.
I
A
(equiareal) = min
⇔
(10.33)
d
I
A
/
d
Φ
0
=0
,
Search WWH ::
Custom Search