New PDF release: Climatic Change: Implications for the Hydrological Cycle and

By M. Beniston

The fabric provided during this publication covers such varied components as shifts in precipitation styles in a altering worldwide weather, the results for floods or drought, and issues of dealing with water assets under pressure via bad administration practices, overexploitation, and climatic switch. The originality of this paintings is that it brings jointly less than one hide matters which are usually differently handled in a mono-disciplinary demeanour, i.e. both during the actual sciences or via financial or social concerns. during this manner, the publication has an further price for scientists who desire to increase their horizons and avenues of analysis. The booklet is basically aimed toward complicated educational examine, from PhD or post-doctoral degrees and past.

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Additional info for Climatic Change: Implications for the Hydrological Cycle and for Water Management (Advances in Global Change Research, Volume 10) (Advances in Global Change Research)

Example text

As for the future climate, we find a general increase in the scale parameter, indicating an intensification of heavy precipitation events. In northern and central Europe rather strong increases occur in spring and autumn, while in southern Europe relatively strong increases are found in all seasons but winter peaking in March, July and October, respectively. In all of the three regions the strongest increases occur, however, in autumn, namely in October or November. Changes in the hydrological cycle in Europe 11 The consequences of the aforementioned changes in the two parameters for the precipitation distribution are illustrated in Figure 3, where the probability density functions are shown for Northern Europe in April.

Wilhelm May et al. SOIL MOISTURE For the present-day climate the time-slice experiment reveals the highest soil water content of about 400 mm in a band between about 45 and 55° N including the British Isles, central and eastern Europe (Fig. 9a). Values of about 200 mm occur in southern and northern Europe except for Norway, where the soil water content is about 100 mm due to the high alpine character of this country. The simulation of soil moisture depends crucially in the characteristics of the GCM, in particular on the parameterisations of the soil processes and of the fluxes in the atmospheric boundary layer.

Regarding the maxima of the river discharge or flooding, we find a reduction of up to about 30% for all but one (Don) of the catchments considered. In northern Europe the decrease is due to a reduction of the snow depth in association with the general warming trend and, hence, a reduction of the snow melt in spring. In central and southern Europe the decrease is accounted for by the aforementioned changes in precipitation and evaporation in the respective catchments. The aforementioned changes in the hydrological cycle associated with the climatic change associated with the anticipated increase in the greenhouse gas concentrations have environmental and socio-economic impacts in the European area.

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