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Titlebook: Regional Aspects of Climate-Terrestrial-Hydrologic Interactions in Non-boreal Eastern Europe; Pavel Ya. Groisman,Sergiy V. Ivanov Conferen

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Non-boreal Forests of Eastern Europe in a Changing World: The Role in the Earth Systemchange. Such a program should include system activities directed to improving the ecological state of the region‘s territories and optimizing the structure of agroforestry landscapes, including development of complete systems of protective forests (shelter belts, afforestation of sands and ravine areas, etc.).
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The Northern Eurasia Earth Science Partnership Initiative: An Introductioneochemical cycles, energy and water cycles, and human activities specific to this carbon-rich, cold region interact with global climate. A major concern is that changes in the distribution of land-based life, as well as its interactions with the environment, may lead to a self-reinforcing cycle of a
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Ecological Challenges of Climate Change in Europe’s Continental, Drought-Threatened Southeastonments and with the role of terrestrial vegetation cover according to their importance, although the predicted increase of drought frequency will have a profound effect on quality of human life and on the functioning (“services”) of ecosystems. In this region the southern border of the closed fores
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Climate in the Late Twentieth and Twenty-First Centuries over the Northern Eurasia: RCM and CMIP3 Siture and precipitation output. It has been found that future projections for the extremes in Northern Eurasia are prone to large uncertainties arising primarily from intermodel differences. The uncertainties for “warm” extremes are larger than those for “cold” extremes not only due to greater model-
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An Assessment of the Recent Past and Future Climate Change, Glacier Retreat, and Runoff in the Caucad in summer air temperatures of 0.05°C a. is observed in the high-altitude areas providing for a strong glacier melt and continuous decline in glacier mass balance. A warming of 4–7°C and 3–5°C is projected for the summer months in 2071–2100 under the A2 and B2 emission scenarios respectively, sugge
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Long-Term Forecasting of Natural Disasters Under Projected Climate Changes in Ukrainero-meteorological disasters. This provides the base for more adequate and accurate forecasting of disasters, and to integrate the developed forecasts into the decision making systems. The approach allows the examination of regional risks features in the context of global changes, permits the analysi
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