Skip to main content

Full text: 26: Strömungen und Seegangsverhältnisse vor Graal-Müritz und in der Tromper Wiek

49 
Strömungsstatistik TW3, Record a00008 
Mittel 
Max 
Min 
95%-KI 
Stdabw. 
Varianz 
Ki 
u-Komponente: 
2.04 
18.67 
-7.89 
0.06 
3.24 
10.47 
0.3816xl0 6 
v-Komponente: 
0.11 
12.51 
-9.87 
0.04 
2.32 
5.39 
0.7474x10 s 
Betrag : 
3.83 
18.80 
0.01 
0.04 
2.31 
5.35 
Druck : 
16.22 
17.40 
15.75 
0.00 
0.15 
0.02 
95%-KI = 95% Konfidenzintervall, Stdabw. = Standardabweichung, 
Ki = Eddy Diffusivity IcmVsl 
Meßzeitraum (UTC) 
21.03.2000 08:00 - 03.06.2000 18:50 
Anzahl Messzyklen 
10722 
Messzyklus 
10.00 Minuten 
Messtiefe 
17.0 m 
Bodenabstand 
2.0 m 
Mittlere Richtung 
87 Grad 
Vektorielles Mittel 
2.04 cm/s 
Stabilitaetsfaktor 
53.26 % 
Kovarianz <u'v') 
-2.79 (cm/s) 2 
Kin. Eddy-Energie k e 
7.93 (cm/s) 2 
Mittl. Kin. Energie k m 
2.08 (cm/s) 2 
ke/kn 
3.8 
Hauptachsen-Analyse: 
= 11.7 (cm/s) 2 , A 2 = 4 
1 (cm/s) 2 , 8 * 113.9° (geogr.) 
Prozentuale Häufigkeitsverteilung fuer Speed und Richtung: 
Speedinter 
vall (cm/s) 
0- 
2 
2- 
4 
4- 
6 
6- 
8 
8- 
10 
10- 
12 
12- 
14 
14- 
16 
16- 
18 
18- 
20 
Richtg. 
gesamt: 
0- 30 
Grad 
2.5 
2.8 
1.0 
0.2 
0.1 
0.1 
- 
— 
— 
— 
6.7 
30- 60 
Grad 
2.4 
3.4 
1.1 
0.3 
0.1 
- 
- 
- 
- 
- 
7.3 
60- 90 
Grad 
2.9 
6.4 
4.4 
2.4 
0.9 
0.2 
0.0 
0.0 
0.0 
- 
17.2 
90-120 
Grad 
3.0 
8.3 
7.4 
5.1 
1.6 
0.6 
0.2 
0.3 
0.1 
0.0 
26.6 
120-150 
Grad 
2.2 
4.8 
2.5 
1.3 
0.1 
0.0 
0.0 
- 
- 
- 
10.9 
150-180 
Grad 
1.7 
2.2 
0.4 
0.2 
0.0 
0.0 
- 
- 
- 
- 
4.5 
180-210 
Grad 
1.5 
1.5 
0.1 
0.0 
- 
- 
- 
- 
- 
- 
3.2 
210-240 
Grad 
1.5 
1.3 
0.2 
0.0 
- 
- 
- 
- 
- 
- 
3.0 
240-270 
Grad 
1.3 
1.5 
0.3 
0.0 
- 
- 
- 
- 
- 
- 
3.1 
270-300 
Grad 
1.3 
1.9 
0.4 
0.0 
- 
- 
- 
- 
- 
- 
3.6 
300-330 
Grad 
1.6 
3.0 
1.4 
0.5 
0.3 
0.2 
0.0 
- 
- 
- 
7.0 
330-360 
Grad 
1.6 
2.7 
1.4 
0.6 
0.3 
0.2 
0.1 
- 
- 
- 
6.8 
Speed gesamt 
23.6 
39.6 
20.5 
10.8 
3.5 
1.3 
0.3 
0.3 
0.1 
0.0 
%
	        
Waiting...

Note to user

Dear user,

In response to current developments in the web technology used by the Goobi viewer, the software no longer supports your browser.

Please use one of the following browsers to display this page correctly.

Thank you.