Geography Reference
In-Depth Information
appear when we have a computer at hand. For a large number of map projections, there is no
problem to analytically compute the eigenspace. Such an example is considered after the boxes.
Box 1.9 (Eckert II, the first problem).
x
=
c
1
Λ
4
2
R
√
6
π
,
−
3sin
|
Φ
|
,
1
:=
sign
φ, c
2
:=
R
2
π
3
y
=
c
2
2
−
4
−
3sin
|Φ|
=
πc
1
.
(1.74)
Meridians :
4
x
c
1
Λ
⇒
c
2
c
1
x
Λ
=2
c
2
−
π
x
−
3sin
|
Φ
|
=
y
=2
c
2
−
Λ
,
Λ
= constant
⇒ y
=2
c
2
− c
3
x, c
3
:=
π
Λ
, L
1
(
Λ
= constant)
2
:=
{x ∈
R
|y
=2
c
2
− c
3
x} .
(1.75)
Parallel circles:
Φ
= constant
⇒ x
=
c
4
Λ, c
4
:=
c
1
4
−
3sin
|Φ| ,y
=
c
5
,
c
5
:= 2
c
2
− c
2
4
−
3sin
|Φ| ,
(1.76)
L
1
(
Φ
= constant) :=
2
{
x
∈
R
|
x
=
c
4
Λ, y
=
c
5
}
.
“Half”:
(i) length of the circular equator:
x
(
Λ
=+
π,Φ
=0)
π,Φ
=0)=8
Rπ/
√
6
π,
(ii) length of the central meridian:
x
(
Λ
=0
,Φ
=
π/
2)
−
x
(
Λ
=
−
π/
2) = 4
Rπ/
√
6
π,
−
x
(
Λ
=0
,Φ
=
−
(1.77)
(iii) length of the pole:
=
π/
2) = 4
Rπ/
√
6
π.
x
(
Λ
=+
π,
|
Φ
|
=
π/
2)
−
x
(
Λ
=
−
π,
|
Φ
|
Box 1.10 (Eckert II, the second problem).
x
=
c
1
Λ
4
2
R
√
6
π
,
−
3sin
|
Φ
|
,c
1
:=
sign
φ, c
2
:=
R
2
π
3
y
=
c
2
2
4
−
−
3sin
|
Φ
|
=
πc
1
.
(1.78)
Left Jacobi matrix:
D
Λ
x
=
c
1
4
J
l
:=
D
Λ
xD
Φ
x
,
c
2
Λ
3cos
Φ
sign
Φ
√
4
−
3sin
|Φ|
−
3sin
|
Φ
|
, D
Φ
x
=
−
,
(1.79)
D
Λ
y
=0
,D
Φ
y
=
3
c
2
√
4
−
3sin
|Φ|
cos
Φ
D
Λ
yD
Φ
y
.
Left Cauchy-Green matrix:
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