Abstract
The tendencies of contemporary global and regional climate changes are characterized using long-term data and model simulations in comparison with paleoclimatic reconstructions. The features of climate change in the Arctic and in different Russian regions are noted. The processes that contribute to the climate “nervousness” are considered. The roles of natural and anthropogenic factors in climate change are determined, as well as the ability of numerical models to adequately assess climate change. Global and regional climate trends and their consequences in the 21st century are assessed.
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