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Sinyukovich V.N.,Russian Academy of Sciences | Sizova L.N.,Russian Academy of Sciences | Shimaraev M.N.,Russian Academy of Sciences | Kurbatova N.N.,Irkutsk Center for Hydrometeorology and Environmental Monitoring
Geography and Natural Resources | Year: 2013

We examine the changes in water inflow into Baikal that are taking place due to global warming that enhanced beginning in the 1970s as well as due to the different responses of discharges of separate rivers within the Baikal watershed basin to climate change. © 2013 Pleiades Publishing, Ltd.


Yanchenko N.I.,Irkutsk State University | Slutskii S.L.,Irkutsk Center for Hydrometeorology and Environmental Monitoring | Baranov A.N.,National Research Irkutsk State Technical University | Verkhoturov V.V.,National Research Irkutsk State Technical University
Russian Meteorology and Hydrology | Year: 2015

The variations of the density of atmospheric fallouts of fluorides depending on the source location, sampling period, and research area were subjected to the comparative analysis using the data of snow chemical survey in Bratsk and the results of observations over fluoride atmospheric fallouts in Listvyanka settlement. It is demonstrated that it is reasonable to analyze the actual values of the density of fluoride atmospheric fallouts based on the data of snow chemical survey or plane observations, for assessing the yearly dynamics of the intensity of anthropogenic sources of fluorine. The analysis should account urban (regional) background values, air temperature, and amount of precipitation for the same period of time (the period of stable snow cover or plane observations). © 2015, Allerton Press, Inc.


Sinyukovich V.N.,Russian Academy of Sciences | Kurbatova N.N.,Irkutsk Center for Hydrometeorology and Environmental Monitoring | Chernyavskaya I.A.,Irkutsk Center for Hydrometeorology and Environmental Monitoring
Geography and Natural Resources | Year: 2011

Based on experimental data on the level and elements of the water balance of the Ust'-Ilimsk reservoir, we outline the characteristic properties of the long-term and seasonal regimes of its impounding and drawdown under normal operation conditions (1977-2008). We demonstrate the role played by the individual components of water input and output in the formation of the reservoir's water regime. © 2011 Pleiades Publishing, Inc.

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