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

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,Behördliche Logik bei Risiken und Krisen, of drought is expected to have changed in the last decades. To detect trends regarding drought in forested ecosystems numerous time series of a newly developed ecophysiologically based drought index are analysed. The time series are simulated by the hydrological model WAWAHAMO (WAldWAsserHAushaltsM

Bumble

https://doi.org/10.1007/978-3-322-81089-2ally affects plant physiological processes such as nutrient transport or photosynthesis. These processes in turn partly determine biomass production, plant growth, survival and competition and, thus, vegetation structure. This vegetation-hydrology feedback has the potential to influence the impacts

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SPALL

PANIC

Medientechnik-Theorie oder Medien-Theorie?ed in the subtropical North Atlantic under the influence of the semipermanent high pressure system centered centered at 30°N-40°N in the northeastern Atlantic Ocean. However, the Islands’steep orography makes them much wetter that is usual at these latitudes.

场所

Risikokapital und Aktienfinanzierung. In order to study quantities that vary considerably throughout the Scandinavian area, it is therefore useful to apply a downscaling technique. In this work we will report on investigations of present-day as well as greenhouse-warmed climate over Scandinavia employing a regional climate model (RCM).

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Changes in the mean and extremes of the hydrological cycle in Europe under enhanced greenhouse gas and the ground components. The magnitude of the changes as well as their geographical distribution varies, however, in the course of the year. The magnitude of the changes is largest in autumn, and the regions with an increase or decrease in the respective component are shifted in the meridional di

Excise

,Investigation of the hydrologic cycle simulated by the Canadian Regional Climate Model over the Quéth some overestimation when a lumped hydrologic model is fed by CRCM meteorological outputs. Despite the fact that the hydrologic model was not recalibrated with the CRCM data, this first experience shows the potential use of the CRCM to feed a hydrologic model. In summary, even though our analysis

vasospasm

制造

The GLOWA Volta project: Integrated assessment of feedback mechanisms between climate, landuse, andent of water over the surface and through the atmosphere, three examples are given. The first example treats the indirect and direct effects of changes in soil moisture on the atmospheric circulation. In the second example, the high sensitivity of surface water availability with respect to rainfall