![]() agriculture) between stakeholders, water management measures are implemented since many years. In many protected areas, especially those with existing conflicts of interests (e.g. The local hydrological conditions depend widely on temporal and spatial variations of the main components of the hydrologic cycle and the physiographic conditions on site. Hence, changes in climate are intricately interlinked with changes to the hydrological cycle – the most important feedback cycle in the climate system.įor the management of protected areas knowledge about the water regime plays a very important role, in particular in areas with wetlands, marches or floodplains as well as lakes. Globally, changes in water vapour content of the atmosphere, cloud cover and ice influence the radiation balance of the earth and thus play an important role in determining the climate response to increasing greenhouse gas emissions (Bates et al. It acts as an energy transfer and storage medium through the hydrological cycle. The water cycle is a key process upon which other cycles of the climate system operate. Similarly, water plays a key role in the climatic system. Almost all land-dependent life, habitats and ecosystems depend of freshwater. Changes in hydrology influence plant and animal species in various ways. The dynamics of the water cycle are one of the key variables that determine the distribution and productivity of ecosystems. ![]() Water is involved in all components of the climate system: the atmosphere, hydrosphere, cryosphere, land surface and biosphere. This process is experimental and the keywords may be updated as the learning algorithm improves. These keywords were added by machine and not by the authors. Partly, water resources management can help to counterbalance effects of climate change on stream flow and water availability. This may lead to changes in the water storage, surface runoff, soil moisture and seasonal snow packs as well as to modifications in the mass balance of Central European glaciers. Key changes in the hydrological system include alterations in the seasonal distribution, magnitude and duration of precipitation and evapotranspiration. Generally, an increase in temperature enhances the moisture holding capacity of the atmosphere and thus, leads to an intensification of the hydrological cycle. The hydrological impacts for the protected areas are area-specific and vary from region to region. The following chapter provides an overview of how climate change affects the hydrological regimes in Central and Eastern Europe. ![]() To preserve a favourable conservation status under changing climatic conditions park managers require information about potential impacts of climate change in their area. ![]() The local hydrological conditions depend widely on temporal and spatial variations of the main components of the hydrologic cycle and physiographic conditions on site. For the management of protected areas knowledge about the water regime plays a very important role, in particular in areas with lakes, wetlands, marches or floodplains. ![]()
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