Transformation of spatio-temporal pattern of river regime in Belarus according to climate changes
Keywords:
low-flow period, snow-melting flood, rain flood, precipitation, drought, climate changeAbstract
The paper presents an assessment of current changes in the water regime of rivers in Belarus and possible factors of its transformation. There were established the continuing trends towards an increase in winter low-water river flow, the height of winter floods and a simultaneous decrease in spring streamflow with a decrease in the frequency of floods during the spring flood. These stable trends in the change of river regime in the winter – spring season are associated with an increase in westerly across the Atlantic-European sector since the mid 1960s, which led to mild winters, a decrease in snow cover depth, and an increase in the liquid precipitation amount. Current trends in the change of river regime in the warm season are associated with increased meridional circulation since the mid 1990s, increased aridity and a simultaneous increase in the frequency of heavy rainfall, and, as a consequence, an increase in the minimum flow during the summer – autumn low-water period and the height of rain floods in the eastern half of the country. There has been an increase in the frequency of severe hydrological droughts throughout Belarus, but especially in the western part of the republic due to a significant precipitation deficit in recent decades.
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