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D
l
:=
:= diag[
Λ
min
,Λ
max
]=
0
.
992 10 0
,
(18.36)
0
.
007 97
F
l
=
=
1
.
122 42 1
.
113 55
.
(18.37)
−
0
.
704 30 0
.
709 91
With the help of the left Jacobi matrix
J
l
=
D
Λ
xD
Φ
x
=
−
,
0
.
062 10
−
0
.
996 73
(18.38)
D
Λ
yD
Φ
y
0
.
629 42
−
0
.
082 38
Λ
=6
◦
06
E
,Φ
=50
◦
46
N
the transformation left-to-right is easily performed as
F
r
=J
l
F
l
D
−
l
=J
l
F
l
D
r
=
0
.
770 59 0
.
637 33
,
(18.39)
−
0
.
637 33 0
.
770 59
and
F
r
C
r
F
r
=D
r
,
F
r
G
r
F
r
=F
r
F
r
=I
2
.
(18.40)
Indeed
,
F
r
is an orthonormal matrix.
End of Exercise.
Exercise 18.2 (Bonne projection).
Until recently, the pseudo-conic equal area
Bonne projection
(R. Bonne 1727-1795) was frequently
used for
atlas maps of continents
. The mapping equations are specified through polar coordinates
α
and
r
or Cartesian coordinates
x
and
y
as follows. (
Λ
and
Φ
describe spherical longitude and
spherical latitude.
Φ
0
=60
◦
N is the parallel circle which is mapped isometrically, i.e. without any
distortion.)
cos
Φ
α
=
Λ
Φ
+cot
Φ
0
, r
=
R
(
Φ
0
−
Φ
)+
R
cot
Φ
0
,
(18.41)
Φ
0
−
Φ
+cot
Φ
0
)cos
Λ
,
cos
Φ
x
=
R
(
Φ
0
−
Φ
0
−
Φ
+cot
Φ
0
(18.42)
y
=
R
(
Φ
0
− Φ
+cot
Φ
0
)sin
Λ
.
cos
Φ
Φ
0
−
Φ
+cot
Φ
0
(i) Prove analytically that the Bonne projection is equal area and (ii) determine the numerical
values of the elements of the Tissot indicatrix (Tissot ellipse: minor distortions and major distor-
tions, and coordinates of the corresponding eigendirections in the map) for the point
Alexandria,
Egypt
(
Λ
=29
◦
55
E
,Φ
=31
◦
13
N).
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