Influence of baroclinicity in the atmospheric boundary layer and Ekman friction on the surface wind speed during cold-air outbreaks in the Arctic

Author:

Chechin D. G.,Zabolotskikh E. V.,Repina I. A.,Shapron B.

Publisher

Pleiades Publishing Ltd

Subject

Atmospheric Science,Oceanography

Reference18 articles.

1. B. Brümmer, “Boundary-layer modification in winter-time cold-air outbreaks from the Arctic sea ice,” Boundary-Layer Meteorol. 80 (1), 109–125 (1996).

2. Polar Lows: Mesoscale Weather Systems in the Polar Regions, Ed. by E. A. Rasmussen and J. Turner (Cambridge University Press, Cambridge, 2003).

3. S. Gronas and P. Skeie, “A case study of strong winds at an Arctic front,” Tellus A 51, 865–879 (1999).

4. D. G. Chechin, C. Lupkes, I. A. Repina, and V. M. Gryanik, “Idealized dry quasi 2-D mesoscale simulations of cold-air outbreaks over the marginal sea ice zone with fine and coarse resolution,” J. Geophys. Res. 118 (D16), 8787–8813 (2013).

5. J. E. Overland, R. M. Reynolds, and C. H. Pease, “A model of the atmospheric boundary layer over the marginal ice zone,” J. Geophys. Res. 88 (C5), 2836–2840 (1983).

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