Titlebook: Advances in the Research of Aquatic Environment; Volume 1 Nicolaos Lambrakis,George Stournaras,Konstantina K Book 2011 Springer-Verlag Berl

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Climate change impact on the Almiros brackish karst spring at Heraklion Crete Greeceion height and less, by the precipitation intensity, by the wet day number over the year and by the mean sea level rise, 2) it will not give fresh water during the whole year and sometimes, it will be dried in the summer, 3) due to fractal structure of the limestone porosity, the chloride concentrat

Overthrow

Using spectral analysis for missing values treatment in long-term, daily sampled rainfall time serieyzing the success of the model in order to correctly predict them. The model’s accuracy indicator is built on the basis of a cross correlation function so that time lags of just a few days between observed and predicted values do not affect it. The model performed adequately, especially for the wet

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A GIS method for rapid flood hazard assessment in ungauded basins using the ArcHydro model and the Tattern, highlighting the areas where there is an inherent tendency for higher peak flow rates. In this way, the method allows the detection of locations where higher peak discharge creates a higher flood hazard potential. Results of the method are compared with historical floods damages for verifica

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https://doi.org/10.1007/978-3-031-16329-6e implementation of the WFD, identified and subject to protection as stated in the Basin Water Plans. Therefore, protection elements are common in both directives. The purpose of this paper is directed to conduct a conceptual analysis to define the similarities and differences, and determine the sco

Panacea

Nicolas F. A. J. Carette,Frans van Walree and NAOI, within the rain season of the year (October-March), against a positive correlation within the dry season (April-September). Concerning the temporal distribution of precipitation, decreasing trends appear throughout the Mediterranean, especially in the eastern parts and within the rain sea

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Contemporary Ideas on Ship Stabilitys based on several .C dates combined to a Bayesian age-depth model. Using XRF elemental analysis, we compare the influx of terrestrial material (indicated by K and Rb) to the carbonate precipitation in the lake (indicated by Ca and Sr). The Rb/Sr ratio as a proxy for changes between dry/warm and wet

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