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Greenhouse gases (GHG) concentration in the atmosphere is an important component of the global climate system. It absorbs thermal infrared radiation emitted by the surface of our planet and, thereby, affects the temperature regime of the planet (IPCC, 2001). The atmosphere is a very dynamic system. According to the reports of the Intergovernmental Panel on Climate Change (IPCC), increasing of GHG concentration in the atmosphere that occurred during the last decades, entailed intensification of radioactive forcing of the long-lived GHG by 9% for period 1998–2005 (IPCC, 2007) and by 7.5% for 2005– 2011 (IPCC, 2013). And about 80% of this effect is generated by carbon dioxide (CO2). Terrestrial ecosystems are a major player in interaction between the land surface and the atmosphere. They can release or absorb globally relevant greenhouse gases, and they control exchanges of energy and water between these geospheres (Heimann & Reichstein, 2008). Ecosystems themselves are subject to climatic conditions. They store large amount of carbon in living vegetation, and release of this carbon into the atmosphere could have tremendous consequences. There are two main factors which generate changes in carbon fluxes between the atmosphere and terrestrial ecosystems: i) land use changes (deforestation, irrigation, melioration etc.) and ii) UDC (528.831.1/.4:633.003.13):629.783](4)

Spatio-temporal trend analysis of vegetation productivity in Europe using MODIS data sets