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Climate Factors affecting climate, measuring stations and physical geographic characteristics of the Osogovo Region The territory for which the climate is being defined and meteorological conditions analyzed, embraces the mountainous areas of the Osogovo Mountains massif as well as the northeastern parts of Republic of Macedonia that affect the formation of a specific type of mountainous climate, which has its own climate features. Several groups of influencing factors impact the climate formation of this area, such as: physical-geographic factors, radiation factors, circulation factors as well local factors. The measuring observation network for defining the climate and meteorological conditions on the territory of the Osogovo Mountains, along with their parameters, have been analyzed through data received from the following main climate stations: Stip, Kriva Palanka, Berovo, Kratovo, Kocani, Kumanovo, Sveti Nikole and Delcevo, as well as from several rainfall measurement stations. It must be noted that the spatial distribution of climate and meteorological conditions are not only determined by the size and allocation of the mountainous region and hydrographic and hydrological conditions, but also by the size of the basins and river valleys, the vegetation and pedological conditions, the influence of the general circulation of the atmosphere manifested through changes in airmass, as well as by the impact of solar and astronomical factors. The boundary between the modified continental and continental pluviometric regime (Ristevski P. 1986) lies on this territory, extending on the mountainous regions of the upper river courses of Pcinja and the highest parts of the Osogovo Mountains on one side, the upper courses of the Bregalnica river confluence and northeastern territory of Republic of Macedonia, on the other side, through the influence of the mountain of Kozjak and Siroka Planina that affect the differentiation of the northeastern air-masses and their modification, which in most part are rich in moisture in comparison to other types of northern and northwestern air-masses. Aside from the eastern and northeastern influence of these mountains on the transformation of the air-masses, by the reduction of the moisture they carry with them, these mountains also have an influence on the average changes in air temperatures and changes in other climatic conditions, on the amount of

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Fizibility studija carev vrv english translation  

Fizibility studija carev vrv english translation  

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