Geography Reference
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D l :=
:= diag[ Λ min 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 =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 =31 13 N).
 
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