Titlebook: Global Change and Regional Impacts; Water Availability a Thomas Gaiser,Maarten Krol,Jose C. Araújo Book 2003 Springer-Verlag Berlin Heidelb

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Anna Rywczyńska,Agnieszka Wrzesień) tool to facilitate the integration of the conclusions from the WAVES research into regional land use planning. Scaling techniques were used in the model to extrapolate the largely point-based results of the different WAVES working groups to the entire region. Thus, the model shows the causal link

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https://doi.org/10.1007/978-3-658-39270-3rainfall of about 900 mm competes with a potential evaporation of 2200 mm powered by 3000 h of sunshine. Real evapotranspiration is of the order of 700 mm (SUDENE 1980; corresponding to 78% of rainfall), leaving only about 120 mm (13%) for runoff and 80 mm (9%) for percolation. Specific runoff in th

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https://doi.org/10.1007/978-3-7091-1425-4mong the vegetational types, we may find: vegeta??o da planície litoranea (vegetation of the littoral plain), mata de tabuleiro (forest from the tableland), mata de dunas (forest from the dunes), manguezal (mangroves), caatinga (stunted sparse forest), cerrado (open pasture with patches of stunted v

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https://doi.org/10.1007/978-3-8349-9364-9 the form as this has been considered. The current estimates reveal, in spite of the superpositions, that few of the vegetal formations of the state are being protected, not guaranteeing the necessary minimum for the conservation of the tropical biota. The caatinga and the cerrado are the great phyt

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Methods of Data and Software Migration,l, generated by a dynamic mode1ing approach. The second is to elaborate a state-of-the-art regional-scale climate model, which can be applied to simulate scenarios of future climatic developments in the northeast of Brazil. For this, two different types of such models were adapted to the region of i