20-1 Geodesic, geodesic circle, Darboux frame, Riemann coordinates 423
Example 20.2 (Geodesic as a submanifold in {E
2
A 1 ,A 2
, G KL }, B = c = const: “parallel circle”).
X = +E 1
A 1 cos c cos T
1 − E 2 sin
2 c
+ E 2
A 1 cos c sin T
1 − E 2 sin
2 c
+ E 3
A 1 (1 − E
2 ) sin c
1 − E 2 sin
2 c
,
(20.38)
D 1 = −E 1 sin T + E 2 cos T =: ˙
X/ ˙
X ,
D 2 = −E 1 sin c cos T − E 2 sin c sin T + E 3 cos c ,
D 3 = +E 1 cos c cos T + E 2 cos c sin T + E 3 sin c ,
(20.39)
D =
⎡
⎢
⎢
⎣
− sin T
cos T
0
− sin c cos T − sin c sin T cos c
cos c cos T
cos c sin T sin c
⎤
⎥
⎥
⎦ E ,
D = RE , D
= R
E = R
R
T D = ΩD ∀ R ∈ SO(3) ,
R
=
⎡
⎢
⎢
⎣
−T
cos T
−T
sin T
0
+T
sin c sin T −T
sin c cos T 0
−T
cos c sin T +T sin c cos T 0
⎤
⎥
⎥
⎦ ,
Ω := R
R
T =
⎡
⎢
⎢
⎣
0
+T
sin c −T
cos c
−T
sin c
0
0
+T
cos c
0
0
⎤
⎥
⎥
⎦ ,
(20.40)
κ g = +T
sin c , κ n = −T
cos c , τ g = 0 ,
˙
X =
dS
dT
=
A 1 cos c
1 − E 2 sin
2 c
,
T
:=
dT
dS
=
1 − E 2 sin
2 c
A 1 cos c
⇒
κ g = +
1 − E 2 sin
2 c
A 1
tan c = const ,
κ n = −
1 − E 2 sin
2 c
A 1
= const ,
τ g = 0 .
(20.41)
End of Example.
Obviously, the parallel circle B = const is a geodesic circle. Note that for a sphere S
2
R great circles
are geodesics, but small circles are geodesic circles. Following the curvature measure representation in
Corollary 20.1, we can characterize geodesics and geodesic circles by differential equations.
Example 20.2 (Geodesic as a submanifold in {E
2
A 1 ,A 2
, G KL }, B = c = const: “parallel circle”).
X = +E 1
A 1 cos c cos T
1 − E 2 sin
2 c
+ E 2
A 1 cos c sin T
1 − E 2 sin
2 c
+ E 3
A 1 (1 − E
2 ) sin c
1 − E 2 sin
2 c
,
(20.38)
D 1 = −E 1 sin T + E 2 cos T =: ˙
X/ ˙
X ,
D 2 = −E 1 sin c cos T − E 2 sin c sin T + E 3 cos c ,
D 3 = +E 1 cos c cos T + E 2 cos c sin T + E 3 sin c ,
(20.39)
D =
⎡
⎢
⎢
⎣
− sin T
cos T
0
− sin c cos T − sin c sin T cos c
cos c cos T
cos c sin T sin c
⎤
⎥
⎥
⎦ E ,
D = RE , D
= R
E = R
R
T D = ΩD ∀ R ∈ SO(3) ,
R
=
⎡
⎢
⎢
⎣
−T
cos T
−T
sin T
0
+T
sin c sin T −T
sin c cos T 0
−T
cos c sin T +T sin c cos T 0
⎤
⎥
⎥
⎦ ,
Ω := R
R
T =
⎡
⎢
⎢
⎣
0
+T
sin c −T
cos c
−T
sin c
0
0
+T
cos c
0
0
⎤
⎥
⎥
⎦ ,
(20.40)
κ g = +T
sin c , κ n = −T
cos c , τ g = 0 ,
˙
X =
dS
dT
=
A 1 cos c
1 − E 2 sin
2 c
,
T
:=
dT
dS
=
1 − E 2 sin
2 c
A 1 cos c
⇒
κ g = +
1 − E 2 sin
2 c
A 1
tan c = const ,
κ n = −
1 − E 2 sin
2 c
A 1
= const ,
τ g = 0 .
(20.41)
End of Example.
Obviously, the parallel circle B = const is a geodesic circle. Note that for a sphere S
2
R great circles
are geodesics, but small circles are geodesic circles. Following the curvature measure representation in
Corollary 20.1, we can characterize geodesics and geodesic circles by differential equations.
