RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 20, ES1001, doi:10.2205/2019ES000684, 2020
Figure 6. Trajectories of air particles in the upper layers of the flow around the middle relief for the options: a) $\lambda_c = 5$, $U = 10.01$, $\gamma_j = 6, \:0,\: 3$ (thin lines); b) $\lambda_c = 5$, $U = 11.11$, $\gamma_j= 5,\: 0, \:3$ (bold dotted line). Trajectories with $z_0 = 10 \: (0.5)\: 30$ are presented.
Citation: Kozhevnikov V. N., R. B. Berzegova, M. K. Bedanokov (2020), Modeling of the Novorossiysk bora. Part 1. Atmospheric disturbances over the mountains of Novorossiysk, Russ. J. Earth Sci., 20, ES1001, doi:10.2205/2019ES000684.
Copyright 2020 by the Geophysical Center RAS.
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