Titlebook: Climatic Change: Implications for the Hydrological Cycle and for Water Management; Martin Beniston Book 2002 Springer Science+Business Med

onlooker

Wolfgang Gerke,Christof Aignesberger. (1994), and in a region representative for the Romania zone (ROMZ)..In order to test the influence of NAO (North Atlantic Oscillation) or ENSO (El Nino- Southern Oscillation) on the precipitation fields or on the drought index, the correlation technique has been applied using the lags from 1 to 12

放纵

https://doi.org/10.1007/978-3-8350-9045-3ncapsulated in any climate change impacts assessment. The initial source, that of emissions scenarios derived from socio-economic projections is described and from here the cascade of the probable ranges of uncertainty associated with each step in an impacts assessment study is discussed. This asses

COWER

https://doi.org/10.1007/978-3-8350-9045-3cs provides the necessary background. Hydropower production for urban areas and irrigation development in rural areas compete for water resources. The paper introduces the GLOWA Volta project and presents details highlighting the project’s integrative approach. In order to address water-policy issue

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overshadow

https://doi.org/10.1007/978-3-8350-9045-3arly, the main course of the lower reaches has been drying up which has caused a series of ecological, environmental and socioeconomical problems. In this paper, we have tried to explain the reasons for the hydrological cycle changes regarding the physical aspects and human activities. On the basis

Conjuction

https://doi.org/10.1007/978-3-8350-9045-3. If this assumption is incorrect then the existing design procedures for embankments, dams, reservoirs, relief channels, polders, etc. will have to be revised. Without revision, the flood protection systems can be over- or under-designed and either not serving their purpose adequately or being over

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