Geography Reference
In-Depth Information
(“spherical isometric latitude”)
.
Second standard integral:
E
2
1
−
d
Φ
cos
Φ
=
I
second
.
(9.40)
E
2
sin
2
Φ
1
−
E
cos
Φ
1+
E
sin
Φ
−
,
1
− E
2
1
cos
Φ
=
1
cos
Φ
−
E
2
E
cos
Φ
(9.41)
E
2
sin
2
Φ
1
−
1
−
E
sin
Φ
1
−
E
2
d
Φ
cos
Φ
=
E
2
sin
2
Φ
1
−
=lntan
π
4
+
Φ
E
2
ln
1+
E
sin
Φ
−
E
sin
Φ
=
2
1
−
ln
tan
π
E/
2
:=
Q
1
4
+
Φ
E
sin
Φ
1+
E
sin
Φ
−
(9.42)
2
(“ellipsoidal isometric latitude”)
.
The combination of the first and the second standard integral leads us to the celebrated relation
in terms of the integration constants
c
and
k
,namely
q
=
a
(
Q
+
k
)
,k
=ln
c, c
=exp
k
;
ln tan
π
=
a
lntan
π
4
+
φ
4
+
Φ
aE
2
ln
1+
E
sin
Φ
−
1
− E
sin
Φ
+
a
ln
c.
(9.43)
2
2
Let us fix the integration constants
a, c
,and
r
. In the so-called “fundamental point”
P
0
(
Λ
0
,Φ
0
),
we assume
r
:=
N
(
Φ
0
), where the curvature form
N
0
is defined by (
9.44
) (“first proposal of C.
F. Gauss”). Around the “fundamental point”
P
0
(
Λ
0
,Φ
0
), we assume the Taylor expansion that is
defined by (
9.45
) (“second proposal of C. F. Gauss”).
A
1
r
=
N
0
=
1
,
(9.44)
E
2
sin
2
Φ
−
ln
Λ
=ln
Λ
0
dln
Λ
d
φ
d
2
ln
Λ
d
φ
2
(
φ − φ
0
)+
1
2
(
φ − φ
0
)
2
+
··· .
(9.45)
φ
0
φ
0
The following three postulates specify the above relations. Note that we can summarize the three
postulates in such a way that we postulate a
horizontal turning tangent
according to Fig.
9.1
.
Search WWH ::
Custom Search