RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 20, ES1001, doi:10.2205/2019ES000684, 2020
| $x$, km | $-$22 | $-$17 | $-$6.75 | $-$6 | $-$3 | 0 | 0.05 | 0.1 | 0.15 | 1.5 | 2.15 | 2.8 |
| $sr$, m | 72 | 96 | 479 | 511 | 255 | 548 | 547 | 544 | 540 | 286 | 161 | 58 |
| $ch$, m | 120 | 173 | 472 | 359 | 249 | 421 | 420 | 417 | 413 | 194 | 101 | 30 |
| $iskV$, m | 72 | 96 | 275 | 285 | 348 | 548 | 547 | 544 | 540 | 286 | 161 | 58 |
| $iskN$, m | 134 | 180 | 284 | 292 | 325 | 350 | 349 | 349 | 349 | 289 | 161 | 58 |
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.