Baltic Sea

More documents

Recommendations

Info

Power Spectral Density Volume transports through Stolpe Channel at 17.5 o E 10 12 for salt > 12 g/kg vol transport all vol transport eastward vol transport westward 10 11 10 10 10 9 10 8 10 7 3 2 1 1=429.16 days 2=321.87 days 3=183.91 days Power Spectral Density Volume transports through Gdansk Basin at 55 o N 10 12 for salt > 12 g/kg vol transport all vol transport northward vol transport southward 10 11 10 10 10 9 1 2 1=429.14 days 2=320.63 days 10 6 10 0 10 1 10 2 10 3 10 4 Period (day) Volume transports through Gdansk Basin at 56 o N 10 13 for salt > 12 g/kg vol transport all vol transport northward vol transport southward 10 12 10 8 10 0 10 1 10 2 10 3 10 4 Period (day) Power Spectral Density 10 11 10 10 2 1 10 9 1=429.16 days 2=321.88 days 10 8 10 0 10 1 10 2 10 3 10 4 Period (day) Figure 5.4: Power Spectra of modelled volume transports of the three transects marked in Fig. 4.18. Stolpe Channel in top left panel, Gdansk Basin in top right panel and Hoburg Channel in lower panel. 114
2 1.5 1 Cumulative volume through Stolpe Channel − 5−day means of salinity < 12 g/kg 2.5 x 104 Date (dd/mm/yy) pos and neg pos neg 4000 3000 2000 Cumulative volume through Stolpe Channel − 5−day means of salinity < 12 g/kg pos and neg pos neg Volume (km 3 ) 0.5 0 −0.5 Volume (km 3 ) 1000 0 −1000 −1 −1.5 −2000 −2 −3000 −2.5 11/10/02 23/02/04 07/07/05 19/11/06 02/04/08 15/08/09 (a) 2002 −2009 −4000 03/05/06 22/06/06 11/08/06 30/09/06 19/11/06 08/01/07 27/02/07 18/04/07 Date (dd/mm/yy) (b) May 2006 −March 2007 1500 Cumulative volume through Stolpe Channel − 5−day means of salinity < 12 g/kg 1000 Volume (km 3 ) 500 0 −500 −1000 pos and neg pos neg −1500 20/09 30/09 10/10 20/10 30/10 09/11 19/11 29/11 09/12 19/12 29/12 Date in 2006 (dd/mm) (c) September to December 2006 Figure 5.5: Cumulative positive (eastward, red), negative (westward, blue) and both positive/negative (black) volume (km 3 ) through Stolpe Channel at 17.5 ◦ E for salt < 12 g/kg; position is marked in Fig. 4.18. Note, scales between plots dier. 115
Page 1 and 2:
No 88 2012 Spatiotemporal Scales of
Page 3 and 4:
Meereswissenschaftliche Berichte MA
Page 5 and 6:
Abstract The Baltic Sea is surround
Page 7 and 8:
Contents Abstract Contents List of
Page 9 and 10:
Acknowledgement 109 Appendix 111 vi
Page 11 and 12:
M-7/M-8 Mesodyn hydrographic snapsh
Page 13 and 14:
List of Figures 1.1 Baltic Sea - ba
Page 15 and 16:
4.32 Regression sea level dierence
Page 17 and 18:
1. Introduction 1.1 Investigations
Page 19 and 20:
circulation above topographic anks
Page 21 and 22:
58 o N 190 230 210 100 75 100 100 7
Page 23 and 24:
y 'new' deep water. For instance, i
Page 25 and 26:
events. During and after such event
Page 27 and 28:
this inow event was classied as 'mo
Page 29 and 30:
Scale (PSS-78), roughly by 0.5%, as
Page 31 and 32:
(Acoustic Doppler Current Proler) a
Page 33 and 34:
for the southernmost zonal section
Page 35 and 36:
whereas the length of the NE time s
Page 37 and 38:
have a thickness of only 1.5 m in o
Page 39 and 40:
dependent salt volumes for the deep
Page 41 and 42:
7 6.5 a Temperature ( o C) 6 5.5 5
Page 43 and 44:
Potential Temperature ( o C) 8 7 6
Page 45 and 46:
inowing waters masses with variable
Page 47 and 48:
following these bounds will be used
Page 49 and 50:
60 80 100 −45 −50 −55 Pressur
Page 51 and 52:
Monitoring Station BMP271 60 80 100
Page 53 and 54:
Date 31.8.1997, 03.11.1997, 03.11.1
Page 55 and 56:
190 a 200 Depth (m) 210 220 230 240
Page 57 and 58:
Date (ID) 〈S〉 V (g/kg) 〈θ〉
Page 59 and 60:
deviation of the temperature uctuat
Page 61 and 62:
4. The Deep Circulation in the EGB
Page 63 and 64:
Depth (m) 50 100 150 200 17 16 4.6
Page 65 and 66:
For this reason, the displayed temp
Page 67 and 68:
6.4 6.3 178 m 208 m 223 m Daily Tem
Page 69 and 70:
The deep parts of the basin are exp
Page 71 and 72:
On the 29 September 2006 between 60
Page 73 and 74:
In the geostrophic balance horizont
Page 75 and 76:
captured eastward velocities up to
Page 77 and 78:
Figure 4.11: Modelled current veloc
Page 79 and 80: SFS and SFN. At the southern ank a
Page 81 and 82: Mean Volume Transports Mean Volume
Page 83 and 84: 160 170 180 Volume of EGB below 170
Page 85 and 86: Basin 55.9 ◦ N. From there the bo
Page 87 and 88: Volume transports (km 3 /d) 15 10 5
Page 89 and 90: Gdansk Basin happened a few weeks e
Page 91 and 92: needs some explanation, since the l
Page 93 and 94: and Fig. 4.24 and displayed in Tabl
Page 95 and 96: Salt (t) 8 6 4 2 0 2 4 6 8 x 10 10
Page 97 and 98: Time Period Stolpe Channel at 17.5
Page 99 and 100: Modelled volume transport through S
Page 101 and 102: discovered that most of the varianc
Page 103 and 104: to the right (perpendicular) to the
Page 105 and 106: of salty and often well oxygenated
Page 107 and 108: Depth (m) 40 45 50 55 60 4 3 2 1 0
Page 109 and 110: a correlation coecient of R=-0.68 a
Page 111 and 112: 5. Discussion and Conclusions 5.1 D
Page 113 and 114: graphic cross-sections, conducted i
Page 115 and 116: direction as the wind. The deep lay
Page 117 and 118: Bibliography Axell, L. B., 1998: On
Page 119 and 120: Griffies, S. M., R. C. Pacanowski,
Page 121 and 122: Matthäus, W., 1993: Major inows of
Page 123 and 124: Rubio, A., D. Gomis, G. Jordà and
Page 125 and 126: Zhurbas, V., I. Oh and V. Paka, 200
Page 127 and 128: Appendix Current speed and directio
Page 129: Current speed and direction (cm/s)
Page 133 and 134: Volume (km 3 ) 2.5 2 1.5 1 0.5 0
Page 135 and 136: 10 3 Regional Wind 7 Power Spectra
Page 137 and 138: NE along−slope at 178m 10 2 10 1
Page 139 and 140: Meereswissenschaftliche Berichte MA
Page 141 and 142: 26 (1997) Lakaschus, Sönke: Konzen
Page 143 and 144: 51 (2002) Wasmund, Norbert; Pollehn
Page 145 and 146: 78 (2009) Wasmund, Norbert; Pollehn
show all

Baltic Sea

Create successful ePaper yourself

Delete template?

Save as template?