ROLUL FACTORULUI CLIMATIC ÎN EVOLUŢIA VERSANŢILOR TÂRNAVEI MARI ÎN SECTORUL COPŞA MICĂ-BLAJ
Role of the climate factors in the evolution of slopes of Târnava Mare river between Blaj and Copşa Mică

Summary/Abstract: With its elements, the climate represents one of most dynamic the external agents with different implications in the dynamism and the mechanism of the natural shaping processes. The quantitative and qualitative analysis of these elements, of their territorial allotment along with the other physical and geographical factors, aloud the knowledge of how the different shaping processes manifest, of the rhythm of the process and of the settlement of the evolution direction of different relief. The Tarnava Mare Valley which located between Copsa Mica and Blaj has a temperate and continental climate which is generally mild and air masses circulation is generally from west. The climate elements influences in a favorable way the practice of different agrarian cultivations, especially grapes in the Blaj area, a cultivation specific to slopes which are orientated south and east. Talking about relief, we distinguish different types of climates such as sunny slope climate or shadowed slope climate, plateau climate or valley bottom climate.

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