Geography Reference
In-Depth Information
we recognize the homogeneous polynomial form of (
H.117
) as soon as we substitute
x
:= sin
Φ
∗
by (
H.118
)and
y
by (
H.119
). The inverse of the univariate homogeneous polynomial (
H.120
)
represented by (
H.121
) is computed up to degree five. Forward and backward substitution amount
to (
H.129
) reevaluated by means of the final solution to the inversion by (
H.131
).
ar tanh
x
=
x
+
x
3
3
+
x
5
5
+
x
7
7
+O(
x
9
)(
|
x
|
<
1)
,
(H.113)
(1 +
x
)
−
1
=1
x
+
x
2
x
3
+O(
x
4
)(
−
−
−
1
<x<
1)
,
(H.114)
2
E
artanh(
E
sin
Φ
∗
)=
1
1
2
sin
Φ
∗
+
1
6
E
2
sin
3
Φ
∗
+
1
10
E
4
sin
5
Φ
∗
+O(
E
6
)
,
(H.115)
sin
Φ
∗
2(1
− E
2
sin
2
Φ
∗
)
=
1
2
sin
Φ
∗
+
1
2
E
2
sin
3
Φ
∗
+
1
2
E
4
sin
5
Φ
∗
+O(
E
6
)
,
(H.116)
sin
Φ
∗
1
2(1
− E
2
sin
2
Φ
∗
)
=sin
Φ
∗
+
2
2
E
ar tanh(
E
sin
Φ
∗
)+
3
E
2
sin
3
Φ
∗
+
3
5
E
4
sin
5
Φ
∗
+O(
E
6
)
.
(H.117)
Equation (
H.65
) can now be written as univariate special homogeneous polynomial of degree
n
,
namely
x
:= sin
Φ
∗
,
(H.118)
y
:=
c
4
1
=
sin
Φ
2
E
ar tanh(
E
sin
Φ
)+
E
2
sin
2
Φ
)
2(1
−
=
c
4
sin
Φ
+
2
5
E
4
sin
5
Φ
+O(
E
6
)
,
3
E
2
sin
3
Φ
+
3
(H.119)
y
(
x
)=
a
11
x
+
a
13
x
3
+
a
15
x
5
+
+
a
1
n
x
n
···
(
n
odd)
,
(H.120)
x
(
y
)=
b
11
y
+
b
13
y
3
+
b
15
y
5
+
+
b
1
n
y
n
···
(
n
odd)
,
(H.121)
subject to
a
11
=1
.
(H.122)
Following
Grafarend
(
1996
), we can immediately formulate the series expansion with respect to an
upper triangular matrix R
A
truncated up to degree five according to (
H.123
) subject to (
H.124
)
as a forward substitution.
⎡
⎤
⎡
⎤
⎡
⎤
⎡
⎤
y
y
3
y
5
1
a
13
a
15
01
a
35
00 1
x
x
3
x
5
x
x
3
x
5
⎣
⎦
=
⎣
⎦
⎣
⎦
+
r
=R
A
⎣
⎦
+
r,
(H.123)
a
13
=
2
3
E
2
,
15
=
3
5
E
4
,
35
=3
a
13
=2
E
2
.
(H.124)
In contrast, the backward substitution leads to (
H.125
)or(
H.126
)
.
⎡
⎤
⎡
⎤
⎡
⎤
⎡
⎤
x
x
3
x
5
1
b
13
b
15
01
b
35
00 1
y
y
3
y
5
y
y
3
y
5
⎣
⎦
=
⎣
⎦
⎣
⎦
+
s
=R
B
⎣
⎦
+
s,
(H.125)
Search WWH ::
Custom Search