Geography Reference
In-Depth Information
7-1 General Mapping Equations
Setting up general equations of the mapping sphere to plane: meta-azimuthal projections in
the oblique aspect. Meta-longitude, meta-latitude.
The general equations for mapping the sphere to the plane using a meta-azimuthal projection
in the oblique aspect involve the most general equations of meta-azimuthal mappings ( 7.1 )in
connection with the constraints ( 7.2 ) for oblique frames of references:
x
y
= r cos α
= f ( B )cos A
,
(7.1)
r sin α
f ( B )sin A
cos Φ sin( Λ
Λ 0 )
tan A =
sin Φ cos Φ 0 ,
cos Φ sin Φ 0 cos( Λ
Λ 0 )
(7.2)
sin B = s Φ cos Φ 0 cos( Λ
Λ 0 )+sin Φ sin Φ 0 .
In order not to mix up the polar coordinate α in the plane and meta-longitude α as introduced in
Chap. 3 ,see( 3.51 )and( 3.53 ), we here refer to A and B as the meta-coordinates meta - longitude
and meta - latitude . In contrast to previous sections, the latitude Φ 0 of the meta-North Pole is not
restricted to Φ 0 =90 (polar aspect) and Φ 0 =0 (transverse aspect), respectively, but can take
all values between Φ 0 =
90 and Φ 0 =90 , i.e. Λ 0
[0 , 360 ]and Φ 0
90 , 90 ].
[
7-2 Special Mapping Equations
Setting up special equations of the mapping “sphere to plane”: the meta-azimuthal pro-
jections in the oblique aspect. Equidistant mapping (oblique Postel projection), conformal
mapping (oblique stereographic projection, UPS), equal area mapping (oblique Lambert
projection).
7-21 Equidistant Mapping (Oblique Postel Projection)
The oblique equidistant mapping of the sphere to a tangential plane is the generalization of
equations derived earlier. The results are stated more precisely in Box 7.1 . Figure 7.2 gives an
impression of the famous oblique equidistant mapping of the sphere to a tangential plane with
the meta-North Pole located in Stuttgart/Germany ( Λ 0 =9 11 0 =48 46 ).
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