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.
The paper considers the features of the mutual influence caused by the ice cover of the Arctic waters and the meridional components of the atmospheric circulation in the Northern Hemisphere of Earth, which are manifested in the modern period. The identification of such features is an urgent problem of climatology, meteorology, oceanography, as well as the maritime transport industry.
The subject of this research is the statistical relationship between interannual changes in a number of characteristics of the Arctic ice cover and components of the atmospheric circulation. The features of the impact of external factors on them are also investigated.
The paper checks the adequacy of the hypothesis put forward that the significant factors of the interannual variability of the characteristics belonging to Arctic Air Outbreak that occur in the summer season in a number of regions of the Arctic include variations in the state of their ice cover caused by the combined effect of global warming and the decline of the average level of solar activity taking place in the current period.
To achieve this goal, there are considered the results of a retrospective analysis of changes in 1993–2019 concerning average daily values of the average thickness of the ice cover, its concentration, average temperature and salinity of the surface layer of the Arctic water areas, as well as air temperatures and meridional components of wind speed in various layers of the troposphere. The specified information has been obtained from the GLORYS, V12, NCEP / NCAR, and ERA - Interim electronic databases. The method of correlation analysis and statistical goodness-of-fit tests were used to assess the adequacy of the hypothesis under consideration.
Using the example of the Arctic waters located in the European, Siberian, Far Eastern and Pacific sectors of the Northern Hemisphere, the features of the mutual influence of changes in the state of their ice cover and meridional components of the atmospheric circulation in the summer season are revea