Titlebook: Climatic Variability in Sixteenth-Century Europe and Its Social Dimension; Christian Pfister,Rudolf Brázdil,Rüdiger Glaser Book 1999 Sprin

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palliative-care

Karin Reisinger,Helmut Pernsteinerare larger than the thermic ones..In the course of the sixteenth century marked cooling phases occurred during all seasons with increasing accentuation. These phases were typical for the climate of the Little Ice Age. In addition to this long-term analysis, some outstanding years of extreme weather

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https://doi.org/10.1007/978-3-658-23480-5st half of the century. Changes in the flooding seasons in both halves of the century are not unambiguous. Results of an analysis on a broader European scale show floods to be a random natural phenomena with limited areal extent defined by the spatial influence of forcing meteorological factors (con

Interregnum

Grundlagen des Risikomanagements, categories are distinguished with storms ranging from one point to eight points. So in the first category the least important storms are given only one point. In category eight the storm surges appear, that have led to the flooding of large areas. These storms are given eight points. As the method

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infinite

978-90-481-5306-0Springer Science+Business Media Dordrecht 1999