Effects of different approximations in 2D-front-scale models on cross frontal structures (weakv ag -case)
Author:
Publisher
Springer Science and Business Media LLC
Subject
Atmospheric Science
Link
http://link.springer.com/content/pdf/10.1007/BF01080877.pdf
Reference33 articles.
1. Andrews, D. G., Hoskins, B. J., 1978: Energy spectra predicted by semi-geostrophic theories of frontogenesis.J. Atmos. Sci.,35, 509?512.
2. Blumen, B., 1980: A Comparison between the Hoskins-Bretherton model of frontogenesis and the analysis of an intense surface frontal zone.J. Atmos. Sci.,37, 64?77.
3. Davies, H. C., Müller, J. C., 1988: Detailed description of deformation-induced semigeostrophic frontogenesis.Quart. J. Roy. Meteor. Soc.,114, 1201?1219.
4. Egger, J., Schmid, S., 1988: Elimination of spurious inertial oscillations in Boundary-Layer Models with time dependent geostrophic winds.Bound.-Layer Meteor.,43, 393?401.
5. Gall, R. L., Williams, R. T., Clark, T. L., 1987: On the minimum scale of surface fronts.J. Atmos. Sci.,44, 2562?2574.
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