Quantification of spurious dissipation and mixing - Discrete variance decay in a Finite-Volume framework

被引:71
作者
Klingbeil, Knut [1 ]
Mohammadi-Aragh, Mahdi [1 ]
Graewe, Ulf [1 ]
Burchard, Hans [1 ]
机构
[1] Leibniz Inst Balt Sea Res, D-18119 Rostock, Germany
关键词
Spurious dissipation; Spurious mixing; Numerical mixing; Variance decay; Advection schemes; Western Baltic Sea; WESTERN BALTIC SEA; OCEAN MODELS; ADVECTION SCHEMES; PART I; FORMULATION; DIFFUSION; CLOSURE; DISCRETIZATION; CONSERVATION; DIAGNOSTICS;
D O I
10.1016/j.ocemod.2014.06.001
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
It is well known that in numerical models the advective transport relative to fixed or moving grids needs to be discretised with sufficient accuracy to minimise the spurious decay of tracer variance (spurious mixing). In this paper a general analysis of discrete variance decay (DVD) caused by advective and diffusive fluxes is established. Lacking a general closed derivation for the local DVD rate, two non-invasive methods to estimate local DVD during model runtime are discussed. Whereas the first was presented recently by Burchard and Rennau (2008), the second is a newly proposed alternative. This alternative analysis method is argued to have a more consistent foundation. In particular, it recovers a physically sound definition of discrete variance in a Finite-Volume cell. The diagnosed DVD can be separated into physical and numerical (spurious) contributions, with the latter originating from discretisation errors. Based on the DVD analysis, a 3D dissipation analysis is developed to quantify the physically and numerically induced loss of kinetic energy. This dissipation analysis provides a missing piece of information to assess the discrete energy conservation of an ocean model. Analyses are performed and evaluated for three test cases, with complexities ranging from idealised 1D advection to a realistic ocean modelling application to the Western Baltic Sea. In all test cases the proposed alternative DVD analysis method is demonstrated to provide a reliable diagnostic tool for the local quantification of physically and numerically induced dissipation and mixing. (C) 2014 Elsevier Ltd. All rights reserved.
引用
收藏
页码:49 / 64
页数:16
相关论文
共 60 条
[11]   Energy-conserving discretisation of turbulent shear and buoyancy production [J].
Burchard, Hans .
OCEAN MODELLING, 2002, 4 (3-4) :347-361
[12]  
Burchard H, 2013, NOTES NUMER FLUID ME, V120, P89
[13]  
Canuto VM, 2001, J PHYS OCEANOGR, V31, P1413, DOI 10.1175/1520-0485(2001)031<1413:OTPIOP>2.0.CO
[14]  
2
[15]   Reducing numerical diffusion in interfacial gravity wave simulations [J].
Fringer, OB ;
Armfield, SW ;
Street, RL .
INTERNATIONAL JOURNAL FOR NUMERICAL METHODS IN FLUIDS, 2005, 49 (03) :301-329
[16]   Diagnostics of diapycnal diffusion in z-level ocean models. Part II: 3-Dimensional OGCM [J].
Getzlaff, Julia ;
Nurser, George ;
Oschlies, Andreas .
OCEAN MODELLING, 2012, 45-46 :27-36
[17]   Diagnostics of diapycnal diffusivity in z-level ocean models part I: 1-Dimensional case studies [J].
Getzlaff, Julia ;
Nurser, George ;
Oschlies, Andreas .
OCEAN MODELLING, 2010, 35 (03) :173-186
[18]   The future of the western Baltic Sea: two possible scenarios [J].
Graewe, Ulf ;
Friedland, Rene ;
Burchard, Hans .
OCEAN DYNAMICS, 2013, 63 (08) :901-921
[19]   Storm surges in the Western Baltic Sea: the present and a possible future [J].
Graewe, Ulf ;
Burchard, Hans .
CLIMATE DYNAMICS, 2012, 39 (1-2) :165-183
[20]  
Griffies SM, 2000, MON WEATHER REV, V128, P538, DOI 10.1175/1520-0493(2000)128<0538:SDMAWA>2.0.CO