Baltic Sea

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Acknowledgement First and foremost, I would like to thank my advisor, Dr. Eberhard Hagen for his constant support and encouragement on this research project. Then I would like to thank Dr. Torsten Seifert and Dr. Martin Schmidt for their support on the model, providing me with model data and introducing me to Ferret. Without Günter Plüschke, Toralf Heene and the crew of the Professor Albrecht Penck the measuring campaigns would have not been possible. Thanks to the IT department for their support and providing me with data from the IOW data base. Then I would like to thank Dr. Lars Umlauf and my fellow PhD students from room 214 for our fruitful discussions. Then I would like to thank my thesis committee, Dr. Rainer Feistel, Dr. Falk Pollehne and Dr. Klaus Peter Koltermann for their help and advice. Furthermore I would like to thank all other friends and colleagues from my time in Rostock and IOW I haven't mentioned so far. I would like to thank Dr. Birgit Klein for her proof reading and advice. Holger Giese was very helpful in the initial stages of the project and provided me with instrumentation. Dr. Ivan Kuznetsov and Dr. Mayya Gogina helped to get the thesis printed and submitted. Dr. Sunke Schmidtko I would like to thank for his proof reading. In my new work at the Scottish Environment Protection agency my boss Dr. Alan Hills and colleague Dr. Ted Schlicke supported me during the writing up period and thanks to all my other friends at SEPA. I would also like to thank my family and friends I haven't mentioned yet for their moral support and understanding over these years. Thanks to the reviewers and to the Deutsche Forschungsgemeinschaft, who funded this project "Tiefe Randströmungen im Östlichen Gotlandbecken der Ostsee", HA 1900/ 3-1/2. 110
Appendix Current speed and direction (cm/s) 50 30 10 10 0 30 Mooring SEcurrent meter 170 m + 175 m 50 03/05/06 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 175 m Current speed and direction (cm/s) 50 30 10 10 0 30 50 Mooring SEcurrent meter at 200 m + 205 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 200 m Current speed and direction (cm/s) 50 30 10 10 0 30 Mooring SEcurrent meter at 215 m + 220 m 50 03/05/06 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 220 m Figure 5.1: Stick plot of currents mooring SE. Hourly values (red), daily values (blue). 111
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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
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: Zhurbas, V., I. Oh and V. Paka, 200
Page 129 and 130: Current speed and direction (cm/s)
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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