100
T. Torsvik
is established after about a decade of simulated time. For regional scale models the
spin-up time is much shorter, particularly if the model domain is influenced by large
water exchange across open lateral boundaries.
For readers who wish to learn more about numerical ocean modelling, Haidvogel
and Beckmann (1999) provide a good overview of the basic concepts. For further
information on how to run ocean models, the best and most up-to-date information
is usually available on the web sites and in the user manuals for each model, so no
references on this subject will be included here.
Acknowledgements This work, originally motivated by the BONUS project BalticWay, was
supported by the European Union through the Mobilitas grant MTT63 and through support to
the Estonian Centre of Excellence for Non-linear Studies (CENS) from the European Regional
Development Fund, and by targeted financing by the Estonian Ministry of Education and Research
(grant SF0140007s11).
References
Anderson JD Jr (1995) Computational fluid dynamics: the basics with applications. McGraw-Hill,
New York
Benestad RE, Hanssen-Bauer I, Chen D (2008) Empirical–statistical downscaling. World Scientific, Singapore
Ferziger JF, Peri´ c M (2002) Computational methods for fluid dynamics, 3rd edn. Springer, Berlin
Haidvogel DB, Beckmann A (1999) Numerical ocean circulation modeling. Imperial College
Press, London
Johnson C (2009) Numerical solution of partial differential equations by the finite element method.
Dover, New York
Joint Panel on Oceanographic Tables and Standards [JPOTS] (1991) Processing of oceanographic
station data. Unesco, Paris. ISBN 9231027565/9789231027567
LeVeque RJ (2002) Finite volume methods for hyperbolic problems. Cambridge University Press,
Cambridge
Monaghan JJ (2012) Smoothed particle hydrodynamics and its diverse applications. Annu Rev
Fluid Mech 44:323–346
Reynolds O (1883) An experimental investigation of the circumstances which determine whether
the motion of water shall be direct or sinuous, and the law of resistance in parallel channels.
Philos Trans R Soc Lond Ser A 174:935–982
Thomas JW (1995) Numerical partial differential equations: finite difference methods. Springer,
Berlin
Thorpe SA (2007) An introduction to ocean turbulence. Cambridge University Press, Cambridge
T. Torsvik
is established after about a decade of simulated time. For regional scale models the
spin-up time is much shorter, particularly if the model domain is influenced by large
water exchange across open lateral boundaries.
For readers who wish to learn more about numerical ocean modelling, Haidvogel
and Beckmann (1999) provide a good overview of the basic concepts. For further
information on how to run ocean models, the best and most up-to-date information
is usually available on the web sites and in the user manuals for each model, so no
references on this subject will be included here.
Acknowledgements This work, originally motivated by the BONUS project BalticWay, was
supported by the European Union through the Mobilitas grant MTT63 and through support to
the Estonian Centre of Excellence for Non-linear Studies (CENS) from the European Regional
Development Fund, and by targeted financing by the Estonian Ministry of Education and Research
(grant SF0140007s11).
References
Anderson JD Jr (1995) Computational fluid dynamics: the basics with applications. McGraw-Hill,
New York
Benestad RE, Hanssen-Bauer I, Chen D (2008) Empirical–statistical downscaling. World Scientific, Singapore
Ferziger JF, Peri´ c M (2002) Computational methods for fluid dynamics, 3rd edn. Springer, Berlin
Haidvogel DB, Beckmann A (1999) Numerical ocean circulation modeling. Imperial College
Press, London
Johnson C (2009) Numerical solution of partial differential equations by the finite element method.
Dover, New York
Joint Panel on Oceanographic Tables and Standards [JPOTS] (1991) Processing of oceanographic
station data. Unesco, Paris. ISBN 9231027565/9789231027567
LeVeque RJ (2002) Finite volume methods for hyperbolic problems. Cambridge University Press,
Cambridge
Monaghan JJ (2012) Smoothed particle hydrodynamics and its diverse applications. Annu Rev
Fluid Mech 44:323–346
Reynolds O (1883) An experimental investigation of the circumstances which determine whether
the motion of water shall be direct or sinuous, and the law of resistance in parallel channels.
Philos Trans R Soc Lond Ser A 174:935–982
Thomas JW (1995) Numerical partial differential equations: finite difference methods. Springer,
Berlin
Thorpe SA (2007) An introduction to ocean turbulence. Cambridge University Press, Cambridge