Abstract
Relationships between the bulk Richardson number, B, and other stability parameters were derived for the atmospheric surface layer. Nomograms were constructed, relating the Monin-Obukhov stability parameter, z/L, to B. The nomograms and the graph of Golder (1972) were used to establish various schemes for classifying z/L, B and Ri, in terms of the Pasquill stability classes.
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Zoumakis, N.M., Kelessis, A.G. The dependence of the bulk Richardson number on stability in the surface layer. Boundary-Layer Meteorol 57, 407–414 (1991). https://doi.org/10.1007/BF00120057
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DOI: https://doi.org/10.1007/BF00120057