Baltic Sea

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50 Mooring NEcurrent meter 178 m Current speed and direction (cm/s) 30 10 0 10 30 50 30/09/06 19/11/06 08/01/07 27/02/07 Date (dd/mm/yy) (a) Current meter 178 m 50 Mooring NEcurrent meter 208 m Current speed and direction (cm/s) 30 10 0 10 30 50 30/09/06 19/11/06 08/01/07 27/02/07 Date (dd/mm/yy) (b) Current meter 208 m 50 Mooring NEcurrent meter 223 m Current speed and direction (cm/s) 30 10 0 10 30 50 30/09/06 19/11/06 08/01/07 27/02/07 Date (dd/mm/yy) (c) Current meter 223 m Figure 5.2: Stick plot of currents mooring NE. Hourly values (red), daily values (blue). 112
Current speed and direction (cm/s) Current speed and direction (cm/s) Current speed and direction (cm/s) 50 30 10 10 0 30 50 50 30 10 10 0 30 50 50 30 10 10 0 30 50 Mooring SWcurrent meter at 170 + 168 m 22/06/06 11/08/06 30/09/06 19/11/06 08/01/07 27/02/07 Date (dd/mm/yy) (a) Current meter 105 m Mooring SWcurrent meter at 200 + 198 m 22/06/06 11/08/06 30/09/06 19/11/06 08/01/07 27/02/07 Date (dd/mm/yy) (b) Current meter 205 m Mooring SWcurrent at 215 + 213 m 22/06/06 11/08/06 30/09/06 19/11/06 08/01/07 27/02/07 Date (dd/mm/yy) (c) Current meter 215 m Figure 5.3: Stick plot of currents mooring SW. Hourly values (red), daily values (blue). 113
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No 88 2012 Spatiotemporal Scales of
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Meereswissenschaftliche Berichte MA
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Abstract The Baltic Sea is surround
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Contents Abstract Contents List of
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Acknowledgement 109 Appendix 111 vi
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M-7/M-8 Mesodyn hydrographic snapsh
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List of Figures 1.1 Baltic Sea - ba
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4.32 Regression sea level dierence
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1. Introduction 1.1 Investigations
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circulation above topographic anks
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58 o N 190 230 210 100 75 100 100 7
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y 'new' deep water. For instance, i
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events. During and after such event
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this inow event was classied as 'mo
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Scale (PSS-78), roughly by 0.5%, as
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(Acoustic Doppler Current Proler) a
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for the southernmost zonal section
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whereas the length of the NE time s
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have a thickness of only 1.5 m in o
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dependent salt volumes for the deep
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7 6.5 a Temperature ( o C) 6 5.5 5
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Potential Temperature ( o C) 8 7 6
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inowing waters masses with variable
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following these bounds will be used
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60 80 100 −45 −50 −55 Pressur
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Monitoring Station BMP271 60 80 100
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Date 31.8.1997, 03.11.1997, 03.11.1
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190 a 200 Depth (m) 210 220 230 240
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Date (ID) 〈S〉 V (g/kg) 〈θ〉
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deviation of the temperature uctuat
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4. The Deep Circulation in the EGB
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Depth (m) 50 100 150 200 17 16 4.6
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For this reason, the displayed temp
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6.4 6.3 178 m 208 m 223 m Daily Tem
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The deep parts of the basin are exp
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On the 29 September 2006 between 60
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In the geostrophic balance horizont
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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: Appendix Current speed and directio
Page 131 and 132: 2 1.5 1 Cumulative volume through 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
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Baltic Sea

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