Sovremennye problemy distantsionnogo zondirovaniya Zemli iz kosmosa, 2015, Vol. 12, No. 6, pp. 35-47
The impact of climate change on mountain landscapes of the North Caucasus
V.V. Vinogradova
1 , T.B. Titkova
1 , E.A. Belonovskaya
1 , R.G. Gracheva
1
1 Institute of Geography RAS, Moscow, Russia
Changes in the boundaries of high-altitude mountain belts can be treated as a proof of climate change. These changes were caused by termination of human activities. The article demonstrates the role of climatic factors in changes of the boundaries and state of sub-alpine landscapes in the North Caucasus, where the transformation of land use system was observed. Heat and moisture are the limiting factors of vegetation existence. The estimate of changes in heat and humidity was made for the territory of 42–44N 42–44.5E using vegetation index (NDVI), the index of vegetation conditions (VCI), Satellite Climatic Extremes Index (SCEI) and the sum of active temperatures (air temperature above + 10 °C). In the foothills moisture decreases, whereas in the middle mountains the increase in moisture is observed. The estimate of the amount of active temperatures and precipitation for the period of modern warming (1981–2010) compared to the previous period (1951–1980) shows the increase of these parameters in the early twenty-first century. These changes cause the increase in vegetation. It is evidenced by the growth of vegetation index (NDVI) and regeneration of natural boundaries of altitude zones at the beginning of the twenty-first century in this area.
Keywords: climate change, mountain landscapes, vegetation index (NDVI), index of vegetation conditions (VCI), satellite climatic extremes index (SCEI), sum of active temperatures
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