RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 20, ES1001, doi:10.2205/2019ES000684, 2020

Table 2. Dependence Between the Maximum Values of the Range of Vertical Displacements of Trajectories From the Initial Levels and the Extreme Values of Temperature Disturbances
$\lambda_c$, km 3 4 5 6 6.7 7 7.5 7.8 9.5 10 12.2
$z_0$, km 2.5 2.0 2.5 4 3.5 4 5 4.5 4.5 6 3
$\Delta \left( \psi'/U \right)$, km 3.2 4.3 3.2 3.6 2.8 2.1 1.8 1.9 3.3 2.9 1.7
$\max T' > 0$ 1.6 2.3 1.9 1.7 1.4 1.2 1.0 1.1 1.6 1.5 1.0
$\min T' < 0$ $-$3.1 $-$4.4 $-$3.4 $-$2.9 2.7 $-$2.4 $-$2.1 $-$2.2 $-$3 $-$2.9 $-$2.1

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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.
 

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