8 Trajectories and Spreading of Observed and Simulated Drifters in the Baltic Sea
279
Hydrological Institute for providing the RCO data as well as help and fruitful discussions about it.
All trajectory simulations have been made using supercomputers maintained by NSC at Linköping
University, Sweden.
References
Andrejev O, Myrberg K, Alenius P, Lundberg PA (2004) Mean circulation and water exchange
in the Gulf of Finland—a study based on three-dimensional modelling. Boreal Environ Res
9:1–16
Andrejev O, Sokolov A, Soomere T, Värv R, Viikmäe B (2010) The use of high-resolution
bathymetry for circulation modelling in the Gulf of Finland. Est J Eng 16:187–210
Bec J, Gawedzki K, Horvai P (2004) Multifractal clustering in compressible flows. Phys Rev Lett
92:224501
Blanke B, Raynaud S (1997) Kinematics of the Pacific Equatorial Undercurrent: an Eulerian and
Lagangian approach from GCM results. J Phys Oceanogr 27:1038–1053
Corell H, Moksnes PO, Engqvist A, Döös K, Jonsson P (2012) Larval depth distribution critically affects dispersal distance and optimum size for marine protected areas. Mar Ecol Prog Ser
467:29–46
Cressman J, Davoudi J, Goldburg W, Schumacher J (2004) Eulerian and Lagrangian studies in
surface flow turbulence. New J Phys 6:53
de Vries P, Döös K (2001) Calculating Lagrangian trajectories using time-dependent velocity
fields. J Atmos Ocean Technol 18:1092–1101
Döös K (1995) Inter-ocean exchange of water masses. J Geophys Res—Oceans 100:13,499–
13,514
Döös K, Meier HEM, Döscher R (2004) The Baltic haline conveyor belt or the overturning circulation and mixing in the Baltic. Ambio 33:261–266
Döös K, Rupolo V, Brodeau L (2011) Dispersion of surface drifters and model-simulated trajectories. Ocean Model 39:301–310
Döös K, Engqvist A (2007) Assessment of water exchange between a discharge region and the
open sea—a comparison of different methodological concepts. Estuar Coast Shelf Sci 74:585–
597
Döscher R, Willén U, Jones C, Rutgersson A, Meier HEM, Hansson U, Graham LP (2002) The development of the regional coupled ocean–atmosphere model RCAO. Boreal Environ Res 7:183–
192
Falkovich G, Gawedzki K, Vergassola M (2001) Particles and fields in fluid turbulence. Rev Mod
Phys 73:913–975
Funkquist F (2001) HIROMB, an operational eddy-resolving model for the Baltic Sea. Bull Mar
Inst Gda´ nsk 28:7–16
Garfield N, Maltrud M, Collins C, Rago T, Paquette R (2001) Lagrangian flow in the California
Undercurrent, an observation and model comparison. J Mar Syst 29:201–220
Garraffo ZD, Mariano AJ, Griffa A, Veneziani C, Chassignet EP (2001) Lagrangian data in a highresolution numerical simulation of the North Atlantic I. Comparison with in situ drifter data.
J Mar Syst 29:157–176
Gästgifvars M, Lauri H, Sarkanen A-K, Myrberg K, Andrejev O, Ambjörn C (2006) Modelling
surface drifting of buoys during a rapidly-moving weather front in the Gulf of Finland, Baltic
Sea. Estuar Coast Shelf Sci 70:567–576
Giudici A, Kalda J, Soomere T (2012) On the compressibility of surface currents in the Gulf of
Finland, the Baltic Sea. In: Proceedings of the IEEE/OES Baltic 2012 international symposium
“Ocean: past, present and future. Climate change research, ocean observation & advanced technologies for regional sustainability”, Klaip˙ eda, Lithuania, May 8–11, 2012. IEEE Press, New
York, 8 pp
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