Архив статей журнала
The paper discusses extreme precipitation recorded at 14 weather stations on the western coast of the Black Sea according to reanalysis data and at two weather stations according to observation data. Comparison of observation data with reanalysis data has been carried out. The relationship between extreme precipitation at each station and elementary circulation mechanisms (ECMs) has been analyzed according to typing by B.L. Dzerdzeevsky, V.M. Kurganskaya and Z.M. Vitvitskaya. The ECMs at which precipitation extremes were observed simultaneously at several stations were identified. It was determined at which ECMs on the western coast of the Black Sea extreme precipitation events occur most often and the multi-year changes in the duration of these ECMs were analysed.
The paper discusses extreme precipitation recorded at 12 meteorological stations on the Eastern Coast of the Black Sea according to reanalysis data and at three stations according to their observations. Comparison of observational data with reanalysis data is carried out. The relationship between extreme precipitations at each station and elementary circulation mechanisms (ECMs) according to typification developed by B.L. Dzerdzeevsky, V.M. Kurganskaya, and Z.M. Vitvitskaya has been analysed. ECMs was revealed, at which precipitation extremes were noted simultaneously at several stations. It has been established at which ECMs on the Eastern coast of the Black Sea extreme precipitation most often occurs, and long-term changes in the duration of these ECMs are analysed.
The paper discusses extreme precipitation recorded at 23 weather stations in the Crimea. Reanalysis data were used. The relationship between precipitation at each station and elementary circulation mechanisms (ECMs) according to B.L. Dzerdzeevsky, V.M. Kurganskaya, and Z.M. Vitvitskaya has been analysed. The ECMs were revealed, at which precipitation extremes were noted simultaneously at several Crimean stations. It has been established at which ECMs in the Crimea, extreme precipitations most often occur and long-term changes in the duration of these ECMs were analysed.