The influence of atmospheric stability on the `Leipzig' boundary-layer structure

Details The influence of atmospheric stability on the `Leipzig' boundary-layer structure The influence of atmospheric stability on the `Leipzig' boundary-layer structure

Feb 1989

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1989bolme..46..207r&link_type=abstract

Boundary-Layer Meteorology, Volume 46, Issue 3, pp.207-227

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The Leipzig wind profile recorded in 1931 has long been considered representative of the wind profile expected in a steady, barotropic flow in the planetary boundary layer over a flat homogeneous surface. As such, the Leipzig data set has been extensively used in the development of computational models for planetary boundary-layer flows. To date, workers have assumed that the effect of stable stratification in the atmosphere over Leipzig was negligible. In the present work, a second-order turbulence closure that explicitly accounts for the effects of stable stratification is used to analyse the Leipzig data. The importance of stable stratification in this near-neutral data set is demonstrated.

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