Geography Reference
In-Depth Information
f =
R 2
1
n sin Φ + 1
2 R 2
n
2 f 2 =
2 c
sin Φ + c.
For the root to be real for all Φ , the integration constant c should fulfill the inequality c ≥ 2 R n .
The general mapping equations thus are given by ( 17.40 )or( 17.41 ), and the general left principal
stretches are given by ( 17.42 ).
=
,
α
r
(17.40)
2 R n sin Φ + c
=
x
y
sin Φ + c cos( )
,
2 R 2
n
(17.41)
sin( )
n
2 R n sin Φ + c
R cos Φ
R cos Φ
Λ 1 =
, Λ 2 =
n
.
(17.42)
2 R 2
n
sin Φ + c
17-231 Equidistance and Conformality on the Circle-of-Contact, Compare with Fig. 17.10
For the reason to map the standard parallel (circle-of-contact) Φ = Φ 0 equidistantly, we claim
that ( 17.43 ) holds, with the consequence that—together with the cone constant n =sin Φ 0
( 17.44 ) is immediately obtained.
n
2 R n sin Φ 0 + c
R cos Φ 0
Λ 1 | Φ = Φ 0 =
=1 ,
(17.43)
c = R 2 (2 + cot 2 Φ 0 ) .
(17.44)
The mapping equations therefore are provided by ( 17.45 )or( 17.46 ). The left principal stretches
are provided by ( 17.47 ).
=
,
α
r
R
(17.45)
2
n sin Φ +cot 2 Φ 0 +2
= R
x
y
n sin Φ +cot 2 Φ 0 +2 cos( )
,
2
(17.46)
sin( )
Λ 1 =
2 n sin Φ + n 2 +1
cos Φ
cos Φ
, Λ 2 =
2 n sin Φ + n 2 +1 .
(17.47)
 
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