Abstract
Oberhuber (1992) has presented a thermodynamic-dynamic sea-ice model coupled to a global ocean general circulation model. In this paper the addition of a snow model is described. A prognostic equation for snow thickness is presented which is forced by snowfall, snowmelt, snow aging, and the flooding of sea ice. Additionally, the total snow-ice heat content is computed. Simulations indicate an asymmetric behaviour of the model Arctic and Antarctic regions. In the Antarctic, it is important to have snow cover to get a reasonable sea-ice simulation. However, in the Arctic snow cover is less important; but, the heat content there plays an important role in the sea-ice simulation.
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References
Bourke, R.H., and R.P. Garrett, 1987: Sea ice thickness distribution in the Arctic Ocean. Cold Regions Science and Technology, 13, 2107–2117.
Bourke, R.H., and R.P. Garrett, 1987: Sea ice thickness distribution in the Arctic Ocean. Cold Regions Science and Technology, 13, 2107–2117.
Hibler, W.D, 1979: A dynamic thermodynamic sea ice model. J. Phys. Oceanogr., 9, 815–846.
Large, W.G., and S. Pond, 1982: Sensible and latent heat flux measurements over the sea. J. Phys. Oceanogr., 12, 464–482.
Legates, D.R., and C.J. Willmott, 1990: Mean seasonal and spatial variability in gauge-corrected, global precipitation. Inter. J. of. Clim., 10, 111–127.
Manabe, S. R.J. Stouffer, M.J. Spelman, and K. Bryan, 1991: Transient responses of a coupled ocean-atmosphere model to gradual changes of atmospheric CO2. Part I: Annual mean response. J. Clim., 4, 785–818.
Mysak, L.A., 1991: Current and future trends in Arctic climate research: Can Changes of the Arctic sea ice be used as an early indicator of global warming? Centre for Climate and Global Change Research Rep. 91–1, McGill University, Montréal, Canada, 27 pp.
Mysak, L.A., 1991: Current and future trends in Arctic climate research: Can Changes of the Arctic sea ice be used as an early indicator of global warming? Centre for Climate and Global Change Research Rep. 91–1, McGill University, Montréal, Canada, 27 pp.
Zwally, H.J, J. C. Comiso, C.L. Parkinson, W.J. Campbell, F.D. Carsey, P. Gloersen, 1983: Antarctic Sea Ice, 1973–1976 Satellite passive-microwave observations. NASA SP-459, National Aeronautics and Space Administration, Washington, D.C., 206 pp.
Zwally, H.J., A.C. Brenner, J.A. Major, R.A. Bindschadler, J.G. Marsh, 1989: Growth of Greenland ice sheet: Measurement. Science, 246, 1587–1589.
Washington, W.M., and G.A. Meehl, 1989: Climate sensitivity due to increased CO2: experiments with a coupled atmosphere and ocean general circulation model. Clim. Dyn., 4, 1–38.
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© 1993 Springer-Verlag Berlin Heidelberg
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Oberhuber, J.M., Holland, D.M., Mysak, L.A. (1993). A Thermodynamic-Dynamic Snow Sea-Ice Model. In: Peltier, W.R. (eds) Ice in the Climate System. NATO ASI Series, vol 12. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-85016-5_37
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DOI: https://doi.org/10.1007/978-3-642-85016-5_37
Publisher Name: Springer, Berlin, Heidelberg
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