Geography Reference
In-Depth Information
Fig. 8.15.
The ratio
r/
X
P
−
X
c
−
X
P
−
X
c
|
n
n
=
H
0
/
|
X
P
−
X
c
|
n
|
In the next phase, we compute the rectangular coordinates
x
p
and
y
p
as well as the angular
parameters
r
=(
x
∗
p
+
y
∗
p
)
1
/
2
and
α
= arctan
y
p
/x
p
, taking advantage of the ray condition. In
Fig.
8.15
, the principle situation is illustrated.
x
p
=
−
H
0
E
1
∗
|
X
P
−
X
0
x
p
=
E
1
∗
|
X
p
−
X
0
y
p
=
X
P
−
X
0
|
n
−H
0
y
p
=
−
H
0
E
2
∗
|
X
P
−
X
0
⇒
,
(8.108)
E
2
∗
|
X
p
−
X
0
X
P
−
X
0
|
n
−H
0
α
= arctan
E
2
∗
|
X
p
−
X
0
,
(8.109)
E
1
∗
|
X
p
−
X
0
r
H
0
=
=
|
λ
|
X
P
−
X
c
−
X
P
−
X
c
|
n
,
n
|
X
P
−
X
c
|
n
|
⇒
(8.110)
r
=
H
0
X
P
−
X
c
2
−
X
P
−
X
c
|
n
2
.
|
X
P
−
X
c
|
n
|
In Box
8.10
, the computational products are listed. As it is sketched in Box
8.10
, the angular
parameter
r
can be rewritten as (
8.111
).
r
=
H
0
X
P
−
X
0
2
−
X
P
−
X
0
|
n
2
.
(8.111)
|
X
P
−
X
0
|
n
−H
0
|
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