Temporal Characteristics and Synoptic Conditions of Extreme Bora Formation in Novorossiysk
V. V. Efimov✉, O. I. Komarovskaya, T. M. Bayankina
Marine Hydrophysical Institute, Russian Academy of Sciences, Sevastopol, Russian Federation
✉ e-mail: vefim38@mail.ru
Abstract
Purpose. Bora in Novorossiysk is the strong, cold, gusting northeast wind directed to the sea on a ridge slope. As the dangerous phenomenon of weather it happens in winter at the wind speed more than 30 m/s, therefore, bora cases with maximum speed and minimum subzero temperature are of practical and all-physical interest.
Methods and Results. According to long-term daily data from the archives at the station Novorossiysk and observations from the Russian Hydrometeorological Institute (https://rp5.ru/) for the period 1901–2017 statistics on the number of days with bora for cold and warm periods and the number of bora cases with different duration of the day and their repeatability by month for the period 1901‒2017 are obtained. Modern regional numerical models developed in the Marine Hydrophysical Institute permit to take into account the role of orography in generation of the Novorossiysk bora, to define its localization and to study evolution of thermodynamic fields of a strong bora during its development and attenuation. The estimation of the repeatability of extreme wind speeds at true bora by the method of approximation of the cumulative function of the series by the Weibull distribution is given. In the analysis of sinoptic features of bora formation, the data of RegCM regional reanalysis for the period 1979–2013, as well as data of ERA Interim reanalysis at model levels were used. Roses of winds for points at windward and leeward slopes are constructed.
Conclusions. It was found that the average annual number of days with bora for the study time series is 30. The greatest duration of cases with bora falls on the winter months and can be up to 7 days. From the arrays of reanalysis data, the fields of pressure and wind speed corresponding to a strong bora are selected and classified by the cluster analysis method. Composites of pressure and wind fields are constructed. It is shown that the condition for the development of a strong bora is the formation of two pressure centers – the northern cyclonic and southern anticyclonic. Vertical profiles of temperature, wind speed and buoyancy frequency for 2 main clusters are presented. According to the measurements on the Novorossiysk HMS, the time characteristics of the bora were estimated. It is shown that the main features necessary for the formation of a true bora is an intense low – atmospheric air flow with velocities of about 10-15 m/c, accompanied by temperature inversion at an altitude of about 1 km and the formation of the underlying layer of stably stratified air.
Keywords
bora in Novorossiysk, repeatability, cluster analysis, Froude number, buoyancy frequency
Acknowledgements
The investigation is carried out within the framework of the state task on the theme No. 0827-2018-0001 “Fundamental studies of the interaction processes in the ocean-atmosphere system conditioning the regional spatial-temporal variability of natural environment and climate” (code “Ocean and atmosphere interaction”).
Original russian text
Original Russian Text © V. V. Efimov, O. I. Komarovskaya, T. M. Bayankina, 2019, published in MORSKOY GIDROFIZICHESKIY ZHURNAL, Vol. 35, Iss. 5, pp. 409–422 (2019)
For citation
Efimov, V.V., Komarovskaya, O.I. and Bayankina, T.M., 2019. Temporal Characteristics and Synoptic Conditions of Extreme Bora Formation in Novorossiysk. Physical Oceanography, 26(5), pp. 361-373. doi:10.22449/1573-160X-2019-5-361-373
DOI
10.22449/1573-160X-2019-5-361-373
References
- Gusev, A.M., ed., 1959. [Bora of Novorossiysk]. In: MHI, 1959. [Proceedings of the Marine Hydrophysical Institute]. Moscow: AS USSR Publ. Vol. 14, 140 p. (in Russian).
- Vasiliev, A.A., Vil’fand, R.M. and Golubev, A.D., 2016. The Joint Use of Mesoscale Numerical and Conceptual Models in Operational Forecast of Hazard Weather Phenomena. In: A. A. Vasiliev, Ed., 2016. Proceedings of Hydrometcentre of Russia. Мoscow: Hydrometcentre of Russia. Iss. 359, pp. 48-57. Available at: http://method.meteorf.ru/publ/tr/tr359/vasiliev.pdf [Accessed: 20 March 2019] (in Russian).
- Gavrikov, A.V. and Ivanov, A.Y., 2015. Anomalously Strong Bora over the Black Sea: Observations from Space and Numerical Modeling. Izvestiya, Atmospheric and Oceanic Physics, [e-journal] 51(5), pp. 546-556. https://doi.org/10.1134/S0001433815050059
- Vil’fand, R.M., Rivin, G.S .and Rozinkina, I.A., 2010. COSMO-RU System of Nonhydrostatic Mesoscale Short-range Weather Forecast of the Hydrometcenter of Russia: the First Stage of Realization and Development. Russian Meteorology and Hydrology, [e-journal] 35(8), pp. 503-514. https://doi.org/10.3103/S1068373910080017
- Efimov, V.V. and Barabanov, V.S., 2013. Simulation of Bora in Novorossiysk. Russian Meteorology and Hydrology, [e-journal] 38(3), pp. 171-176. https://doi.org/10.3103/ S1068373913030059
- Efimov, V.V. and Komarovskaya, O.I., 2018. Seasonal Variability and Hydrodynamic Regimes of the Novaya Zemlya Bora. Izvestiya, Atmospheric and Oceanic Physics, [e-journal] 54(6), pp. 581-593. https://doi.org/10.1134/S0001433818060051
- Anisimov, A.E., Yarovaya, D.A. and Barabanov, V.S., 2015. Reanalysis of Atmospheric Circulation for the Black Sea-Caspian Region. Physical Oceanography, [e-journal] (4), pp. 13-25. doi:10.22449/1573-160X-2015-4-13-25
- Dee, D.P., Uppala, S.M., Simmons, A.J., Berrisford, P., Poli, P., Kobayashi, S., Andrae, U., Balmaseda, M.A., Balsamo, G. and Bauer, P. [et al.], 2011. The ERA-Interim Reanalysis: Configuration and Performance of the Data Assimilation System. Quarterly Journal of the Royal Meteorological Society, [e-journal], 137(656), pp. 553-597. doi:10.1002/qj.828
- Shaimardanov, V.M., 2011. Organization of Quality Control of Information Including in the Data Fund. In: V. M. Kattsov, E. L. Genihovich, A. S. Zaitsev, I. L. Karol, N. V. Kobysheva, V. P. Meleshko, A. V. Mescherskaya, O. M. Pokrovcky and C. C. Chicherin, eds., 2011. Proceedings of Voeikov Main Geophysical Observatory. Vol. 564, pp. 166-177 (in Russian).
- Alpers, W., Ivanov, A. and Horstmann, J., 2009. Observations of Bora Events over the Adriatic Sea and Black Sea by Spaceborne Synthetic Aperture Radar. Monthly Weather Review, [e-journal] 137(3), pp. 1150-1161. https://doi.org/10.1175/2008MWR2563.1
- Semenov, E.K., Sokolikhina, N.N. and Sokolikhina, E.V., 2013. Meteorological and Synoptic Aspects of the Formation and Evolution of the Novorossiysk Bora. Russian Meteorology and Hydrology, [e-journal] 38(10), pp. 661-668. https://doi.org/10.3103/S1068373913100026
- Hartigan, J.A. and Wong, M.A., 1979. Algorithm AS 136: A K-Means Clustering Algorithm. Journal of the Royal Statistical Society. Series C (Applied Statistics), [e-journal] 28(1), pp. 100-108. https://doi.org/10.2307/2346830
- Smith, R.B., 1989. Hydrostatic Airflow over Mountains. Advances in Geophysics, [e-journal] 31, pp. 1-41. doi:10.1016/S0065-2687(08)60052-7
- Eckermann, S.D., Lindeman, J., Broutman, D., Jun, Ma and Boybeyi, Z., 2010. Momentum Fluxes of Gravity Waves Generated by Variable Froud Number Flow over Three-Dimentional Obstacles. Journal of the Atmospheric Sciences, [e-journal] 67(7), pp. 2260-2278. https://doi.org/10.1175/2010JAS3375.1