Dynamics of the Atmospheric Boundary Layer in the Mountain-Valley Relief of Adygea

The main part of the territory of the Republic of Adygea is located in the mountain-valley relief. The state of the atmosphere over complex relief is controlled by synoptic-scale processes, mesoscale circulations caused by thermal effects, and turbulent processes. The chapter explores the key features of the structure and dynamics of the atmospheric boundary layer over mountainous terrain. The main features of the mountain-valley circulation, the causes and characteristics of slope and valley winds are presented. Special attention is paid to the Novorossiysk bora and exchange processes over reservoirs. The territory of the Republic of Adygea is unique in terms of the variety of landscapes and can become a good testing ground for a comprehensive study of the features of complex wind circulation and validation of models from eddy-resolving to regional numerical models of weather forecasting. This will contribute not only to improving the quality of weather forecasts and dangerous meteorological phenomena, but also to improving the ecological state of the region through more competent planning of economic activities, taking into account the landscape and climatic features of the region.