региональный климат

In this article considers the nature of the atmospheric circulation in the atlantic-eurasian sector of the hemisphere with the use of multiyear averages maps of the surface of the AT-500 Hpa, corresponding to different periods of state of the climate system (stabilization, the second wave of the global warming). On the basis of the dynamics of change of temperature fields on the average level of the troposphere conclusion is made about the forthcoming changes of winter conditions on the Russian plain

There are considered the basic weather- and climate forcing of synoptic processes in the Lower Volga region. Below shows the dynamics of their changes on a background of global climate trends. It is shown that the cold temperature of the winter months is formed under the influence of the arctic anticyclone. Of the cyclones on the arctic front and of the cyclones on the polar front are formed warmer winter weather conditions

In the present article explores the nature of the circulation in the Atlantic-Eurasian sector of the hemisphere at the average level of the tro­posphere. The change of the pressure field at 500 hPa is observed in natural climatic periods of state the earth’s climate system. Shown the role of circulation in the formation of regional climate in the summer.

Quantitative assessment of the territory continentality is an urgent task, because in the conditions of climate change, the index of continentality can be taken into account when developing geographical forecasts of landscape development. The purpose of this study is to assess the change in the index of continentality of Western Siberia in the conditions of the current trend in climate development. The statistical series of observations on seven meteorological stations in Western Siberia served as the information base of the study.