Articles | Volume 16, issue 3
Atmos. Chem. Phys., 16, 1545–1563, 2016

Special issue: Aerosol-Cloud Coupling And Climate Interactions in the Arctic...

Atmos. Chem. Phys., 16, 1545–1563, 2016

Research article 10 Feb 2016

Research article | 10 Feb 2016

Observations of surface momentum exchange over the marginal ice zone and recommendations for its parametrisation

A. D. Elvidge et al.

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Cited articles

Andreas, E. L.: A relationship between the aerodynamic and physical roughness of winter sea ice, Q. J. Roy. Meteor. Soc., 137, 927–943, 2011.
Andreas, E. L., Tucker, W. B., and Ackley, S. F.: Atmospheric boundary-layer modification, drag coefficient, and surface heat flux in the Antarctic marginal ice zone, J. Geophys. Res.-Oceans, 89, 649–661,, 1984.
Andreas, E. L., Horst, T. W., Grachev, A. A., Persson, P. O. G., Fairall, C. W., Guest, P. S., and Jordan, R. E.: Parametrizing turbulent exchange over summer sea ice and the marginal ice zone, Q. J. Roy. Meteor. Soc., 136, 927–943,, 2010.
Arya, S. P. S.: Contribution of form drag on pressure ridges to the air stress on Arctic ice, J. Geophys. Res., 78, 7092–7099,, 1973.
Arya, S. P. S.: A drag partition theory for determining the large-scale roughness parameter and wind stress on the Arctic pack ice, J. Geophys. Res., 80, 3447–3454,, 1975.
Short summary
Rare aircraft observations of surface momentum flux over the Arctic marginal ice zone provide the best means yet to constrain model representation of MIZ surface roughness. The sensitivity of surface roughness to ice concentration over the Arctic MIZ is presented; these results do not support the values used in many models. However, a leading parameterization scheme (that of Lüpkes et al., 2012) is found to provide a good representation of form drag, after some parameter alterations.
Final-revised paper