Geography Reference
In-Depth Information
Box 21.8 (Decomposition of the synthesis matrix B = B
0
+
h
B
1
+O
2
(
h
2
).).
B=
=
e
2
)
n
+
h
]sin
b
cos
l
(
n
+
h
)cos
b
e
2
)
n
+
h
]sin
b
sin
l
(
n
+
h
)cos
b
[(1
−
[(1
−
sin
l
(
n
+
h
)cos
b
cos
l
(
n
+
h
)cos
b
−
0
−
−
···
(21.43)
[
n
2
(1
−
e
2
)+
mh
]sin
l
m
(
m
+
h
)
[
n
2
(1
−
e
2
)+
mh
]cos
l
m
(
m
+
h
)
sin
b
cos
l
m
+
h
sin
b
sin
l
m
+
h
cos
b
m
+
h
−
−
1
0
0
0
2
×
9
,
···
∈
R
−
[
e
2
m
sin
2
b
+2(1
−
e
2
)
n
]sin
b
cos
b
2(
m
+
h
)(1
−e
2
)
0
e
2
n
sin
b
cos
b
m
+
h
e
2
n
sin
b
cos
b
a
1
(
m
+
h
)
−
−
B
0
:=
=
sin
l
n
cos
b
cos
l
n
cos
b
e
2
)tan
b
cos
l
e
2
)tan
b
sin
l
−
0
−
(1
−
−
(1
−
···
(21.44)
[
n
2
(1
e
2
)] sin
l
m
2
[
n
2
(1
e
2
)] cos
l
m
2
−
−
−
sin
b
cos
l
m
sin
b
sin
l
m
cos
b
m
−
−
,
1
0
0
0
···
e
2
m
sin
3
b
cos
b
+2(1
−
e
2
)
n
sin
b
cos
b
2
m
(1
0
e
2
n
sin
b
cos
b
e
2
n
sin
b
cos
b
a
1
m
−
−
m
−
e
2
)
B
1
:=
=
e
n
tan
b
cos
l
e
n
tan
b
sin
l
sin
l
n
2
cos
b
cos
l
n
2
cos
b
−
0
−
−
···
(21.45)
[
m
2
−
n
2
(1
−
e
2
)] sin
l
m
3
[
n
2
(1
−
e
2
)
−
m
2
]cos
l
m
3
sin
b
cos
l
m
2
sin
b
sin
l
m
2
cos
b
m
2
−
−
.
0
0
0
0
···
[
e
2
m
sin
2
b
+2(1
−
e
2
)
n
]sin
b
cos
b
2
m
2
(1
−e
2
)
e
2
n
sin
b
cos
b
m
2
e
2
n
sin
b
cos
b
a
1
m
2
0
−
Example
21.1
numerically illustrates that for the computation of global
{
L, B
}
from local
{
l,b
}
and from datum parameters
{
t
x
,t
y
,t
z
,α,β,γ,s,δa, δe
2
}
we can neglect
h
B
1
. Accordingly, the
synthesis of
{
L, B
}
is performed by [
L, B
]
T
=[
l,b
]
T
+B
0
[
t
x
,t
y
,t
z
,α,β,γ,s,δa,δe
2
]
T
.
Example 21.1 (Synthesis
of
{
L, B
}
from
{
l,b
}
and
from
datum
parameters
t
x
,t
y
,t
z
,α,β,γ,s,δA,δE
2
{
}
, simulation of impact of local height
h
).
a
1
:= 6
,
377
,
397
.
155 [m]
, e
2
:= 0
.
006674372
, A
1
:= 6
,
378
,
137 [m]
,
E
2
:= 0
.
0066943800229
.
l
=14
◦
,b
=40
◦
,h
= 1000m (assumed)
t
x
,t
y
,t
z
,α,β,γ,s,δA,δE
2
{
}
from first section
.
L
0
=
L
(
l,b
)
13
◦
59
54
.
2696
B
0
=
B
(
l,b
)
40
◦
00
00
.
06944
L
=
L
(
l,b,h
)
13
◦
59
54
.
2704
B
=
B
(
l,b,h
)
40
◦
00
00
.
06942
End of Example.
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