%0 Journal Article %1 Merryfield2003 %A Merryfield, W. J. %A Holloway, G. %D 2003 %J OCEAN MODELLING %K ADVECTION; DIFFUSION; IMPLICIT NUMERICAL SCHEME SMALL TRANSPORT; %N 1 %P 1--15 %T Application of an accurate advection algorithm to sea-ice modelling %V 5 %X Modern numerical sea-ice models contain detailed parameterizations of dynamic and thermodynamic processes affecting ice distribution and thickness. However, nearly all such models advect sea ice in response to wind and ocean forcing using either upstream or centered-difference methods, whose deficiencies are well known. We describe application of the second-order moment advection scheme of Prather J. Geophys. Res. 91 (1986) 6671. In idealized tests this method produces relatively distinct ice edges while maintaining positive ice thicknesses and concentrations. Sensitivity of an Arctic circulation model forced by climatological data is described. Crown Copyright (C) 2002 Published by Elsevier Science Ltd. All rights reserved.

@article{Merryfield2003, abstract = {Modern numerical sea-ice models contain detailed parameterizations of dynamic and thermodynamic processes affecting ice distribution and thickness. However, nearly all such models advect sea ice in response to wind and ocean forcing using either upstream or centered-difference methods, whose deficiencies are well known. We describe application of the second-order moment advection scheme of Prather [J. Geophys. Res. 91 (1986) 6671]. In idealized tests this method produces relatively distinct ice edges while maintaining positive ice thicknesses and concentrations. Sensitivity of an Arctic circulation model forced by climatological data is described. Crown Copyright (C) 2002 Published by Elsevier Science Ltd. All rights reserved.}, added-at = {2009-11-03T20:21:25.000+0100}, author = {Merryfield, W. J. and Holloway, G.}, biburl = {https://www.bibsonomy.org/bibtex/2105ced971e997f17a631a7a372f3f80a/svance}, citedreferences = {BRYAN K, 1969, J COMPUT PHYS, V4, P347 ; EBY M, 1994, CLIM DYNAM, V10, P241 ; FLATO GM, 1993, ATMOS OCEAN, V31, P339 ; GERDES R, 1991, CLIM DYNAM, V5, P211 ; GREGORY A, 2000, COMP ADVECTION SCHEM ; HECHT MW, 2000, OCEAN MODEL, V2, P1 ; HIBLER WD, 1979, J PHYS OCEANOGR, V9, P815 ; KALNAY E, 1996, B AM METEOROL SOC, V77, P437 ; KOENIGLANGLO G, 1994, METEOROL Z, V3, P343 ; LEPPARANTA M, 1985, J GEOPHYS RES, V90, P11899 ; PACANOWSKI RC, 1995, 3 GFDL OC GROUP ; PARKINSON CL, 1979, J GEOPHYS RES, V84, P311 ; PRATHER MJ, 1986, J GEOPHYS RES-ATMOSP, V91, P6671 ; RASCH PJ, 1994, MON WEATHER REV, V122, P1337 ; ROOD RB, 1987, REV GEOPHYS, V25, P71 ; ROTMAN DA, 2001, J GEOPHYS RES-ATMOS, V106, P1669 ; RUSSELL GL, 1981, J APPL METEOROL, V20, P1483 ; SMOLARKIEWICZ PK, 1983, MON WEATHER REV, V111, P479 ; SMOLARKIEWICZ PK, 1984, J COMPUT PHYS, V54, P325 ; STEINER N, UNPUB ESTIMATION WIN ; ZALESAK ST, 1979, J COMPUT PHYS, V31, P335}, interhash = {2098004c41ab394fbb6a5bdd87391e18}, intrahash = {105ced971e997f17a631a7a372f3f80a}, journal = {OCEAN MODELLING}, keywords = {ADVECTION; DIFFUSION; IMPLICIT NUMERICAL SCHEME SMALL TRANSPORT;}, number = 1, owner = {svance}, pages = {1--15}, timestamp = {2009-11-03T20:22:04.000+0100}, title = {Application of an accurate advection algorithm to sea-ice modelling}, volume = 5, year = 2003 }