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

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Climatic Change: Implications for the Hydrological Cycle and for Water Management
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Risikoforschung: Perspektiven und Probleme 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
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Risikojournalismus und Risikogesellschaftth 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
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Risikokapital und Aktienfinanzierungfluxes at the lateral boundaries has been found for the spatial distribution of precipitation, more specifically in the representation of stratiform precipitation..However the finest horizontal resolution used in RCM is about 20 km, which remains too coarse for the forcing of hydrological models, es
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https://doi.org/10.1007/978-3-8350-9045-3ent 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
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Grundlagen des Risikomanagements,velop and validate integration techniques, integrated models and integrated monitoring procedures and to implement them in the network-based Decision Support System DANUBIA. It will contain the essential physical and socio-economic processes required for realistic modelling of water and matter fluxe
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https://doi.org/10.1007/978-3-8350-9045-3. through enhanced emissions of greenhouse gases resulting in the global warming and the related effects. Also natural changes (e.g. in channel morphology, solar activity, ENSO cycle) can play a role. All in all, detection of trends in long time series of flood data is of paramount scientific and pr
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Instrument der Risikokapitalallokation,– 2030 (period B), and 2040 – 2050 (period C). The crop spectrum was restricted to winter wheat, winter barley and silage maize. The physiological effects of increased CO. concentrations on plants were studied considering: adjustment of the potential plant growth rate per unit of intercepted photosy
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,Behördliche Logik bei Risiken und Krisen, that broadly corresponds to Castilla-La Mancha, a region of southeastern Spain (364 × 280 km.). We use a regional climate model (ClimRAMS) with nested grids of 14 km and 3.5 km cell ;size, implemented with a USGS global database of elevation and land cover, and the FAO soil classification database.
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