» 
25 
Wick N1 N2 N3 N4 N5 
Wick N1 N2 N3 N4 N5 
Fig. 9: Phase angles G in degree and amplitudes H in cm of the M 2 and S 2 constituents for tidal elevations in the 
NORA section. 
Table 7 
Amplitudes H and phase angles G of 6 tidal constituents calculated from tide gauge time series of 
the NORA- and MO YENS section and model results from Schwiderski [1979-1981] at the 
respective positions 
Consti 
tuent 
N1 
H G 
N2 
H G 
N3 
H G 
N4 
H G 
N5 
H G 
M8 
H G 
M9 
H G 
cm 
O 
cm 
O 
cm 
O 
cm 
O 
cm 
O 
cm 
o 
cm 
O 
Q, 
NORA/MOVENS 
2.5 
338 
2.2 
340 
1.4 
342 
1.5 
4 
1.7 
0 
3.5 
287 
5.1 
214 
Schwiderski 
3.1 
334 
2.7 
327 
2.3 
319 
2.0 
311 
1.8 
293 
2.1 
344 
1.9 
340 
o, 
NORA/MOVENS 
10.0 
26 
7.9 
33 
6.0 
40 
5.5 
41 
4.6 
40 
11.1 
14 
8.9 
90 
Schwiderski 
9.0 
27 
8.0 
37 
6.5 
44 
5.5 
46 
4.5 
47 
6.0 
34 
5.5 
33 
K, 
NORA/MOVENS 
10.6 
189 
8.8 
191 
7.0 
194 
5.7 
200 
4.6 
203 
7.6 
149 
13.1 
233 
Schwiderski 
9.0 
171 
7.5 
177 
6.0 
185 
4.5 
192 
3.5 
191 
6.0 
167 
5.0 
169 
n 2 
NORA/MOVENS 
14.1 
286 
11.3 
299 
9.7 
302 
8.1 
302 
7.0 
301 
14.5 
258 
4.2 
171 
Schwiderski 
15.0 
291 
12.5 
304 
10.5 
308 
8.5 
310 
6.5 
306 
9.5 
265 
9.5 
266 
M 2 
NORA/MOVENS 
79.4 
314 
64.2 
318 
51.3 
328 
42.4 
329 
34.9 
326 
57.9 
295 
50.9 
295 
Schwiderski 
73.5 
291 
59.5 
309 
49.0 
324 
41.0 
330 
33,0 
328 
42.5 
289 
43.5 
291 
s 2 
NORA/MOVENS 
28.0 
7 
23.0 
11 
19.7 
20 
16.9 
19 
14.2 
17 
31.9 
316 
32.6 
320 
Schwiderski 
23.5 
326 
21.0 
351 
17.0 
3 
15.5 
8 
13.5 
4 
17.0 
319 
17.5 
321