Die harmonische Analyse der Gezeitenbeobachtungen. 70 
A, Uebersicht über die Tiden. 
| 
on 
] 
LA 
S 
© 
| 
a 
wa ler 
= 
af 
— 
- 
[= le 
LS 
© 
a 
8 
Se 
© 
= 
3 
zn 
& 
LA 
S 
© 
Ss 
£ 
X 
3 
= 
La 
= 
| 
zZ 
DD) 
= 
z 
3 
I 
Si 
be 
& 
E 
x 
MC 
m 
. 
< 
SD 
a 
Fir 
Ne 
N 
u 
1 
«€ E 
B ss N 2} 
5 ER = 
5 85 | &® 
a = 8 + 
3° m, KA 
a0, N -_ 
25 SE 
£ 
2% 
= N 
PP 
= 
fe 
* 
2S 
3 
3 
38 
De 
» 
x 
Di 
1 
®. 
A 
5 
ä 
35 | 
2 | 
<oE 
Ya 
3AE 
SE 
„557 
= 
SS 
3% + 
+ © BD, 
Las” 
as 
SS 
27£ 
22° 
“5 & 
a: 
S 
wu 
3 
= 
vn 
nr 
x 
= 
© 
zZ Ss 
+ R 
u & 
5.8 
= © 
SE 
3% 
Mi 
X 
> 
38 
O7 
A 1m 
. 
ad 
a 
es 
Da KK 
5859 | 
=D 
. N 20:5 
5 SM 
A E 
Sg 
| SS 
& 
A = x 
band Ss > 
7 SS | 
(=> SS | & 
ed S& | S 
En [> » 
Neal io] 
m ET 
m 
> 
N 
> | 
zo 
lo 
| = [= |] 
EM 
rt 
X 
& 
en 
= 
CS 
x 
und 
zZ 
3 
C 
Pa 
Zz 
MA 
A 
= | 
z | 
= 
» 
> 
© 
Yale] 
—- 
ang 
Sin 
es 
zl Als] 
} ; 
AL 
a] 
= | Ss 
= | 
? 
A 
N 
MM 
+ 
‚5 
+ 
IS 
+ 
EN 
N 
A 
5 
Ti 
U 
mn 
/ N 
- = Ss 
m MM 3 | 
5 8 | s | 
SE m 5 
m“ 1 N | ; 
a N 
BO 
se 
af a 
N 
ya 
= 
F 
X 
x 
a 
RE 
A 
— 
X 
al 
si | 
"R 
| 
a dee 
. 
E 
x. 
% 
= 
Lo 
FR 
=? 
Bi 
x