11/16/2023 0 Comments Heidelberg germany flood![]() ![]() Concerted Action, Proceedings of the first workshop, Delft, 13 to 15 February 1997, European Commission, Hydrological and Hydrogeological Risks, Luxembourg, 389 pp.Ĭastillo Requena, J. River Basin Modelling, Management and Flood Mitigation. Concerted Action, Proceedings of the first expert meeting, Copenhagen, 10 and 11 October 1996, European Commission, Hydrological and Hydrogeological Risks, Luxembourg, 167 pp.Ĭasale, R., Pedroli, G. 41, Springer Verlag, Berlin, Heidelberg, pp. (eds.), Climatic Variations and Forcing Mechanisms of the last 2000 years, NATO ASI Series, Vol. and Enzi, S.: 1996, ‘The analysis of two bi-millenary series: Tiber and Po river floods’, in Jones, P. (ed.), Solar Output and Climate during the Holocene, Paleoclimate Research 16, Fischer Verlag, Stuttgart, New York, pp. and Enzi, S.: 1995, ‘Climatic features during the Spörer and Maunder minima’, in Frenzel, B. ![]() 13, 249 pp.īrádka, J.: 1967, ‘Meteorologické přičiny povodni ve Slezsku’, Meteorol. Verlauf Ursachen und Folgen derMittelalterlichen und neuzeitlichen Bodenerosion, Bodenprozesse, Modelle and Simulationen, Landschaftsgenese and Landschaftsökologie, Technische Universität Braunschweig, H. J.: 1978, ‘Weather compilation as a source of data for the reconstruction of European climate during the medieval period’, Climatic Change 1, 331-348.īork, H. and Martin-Vide, J.: 1998, ‘Secular climatic oscillations as indicated by catastrophic floods in the Spanish Mediterranean coastal area (14th-19th centuries)’, Climatic Change 38, 473-491.īayerisches Staatsministerium für Landesentwicklung und Umweltfragen: 1985, Wasserwirtschaftliche Rahmenuntersuchung Donau and Main, München, 204 pp.īell, W. 73-83.īarriendos, M.: 1995b, ‘Oscilaciones climaticas seculares a través de las inundaciones catastróficas en el litoral mediterráneo: siglos XIV-XIX’, Estudios Geográficos 56, 223-237.īarriendos, M. (ed.), Situaciones de riesgo climático en España, Instituto Pirenaico de Ecología, Jaca, pp. El episodio de noviembre de 1617 en Catalunya’, in Creus, J. XV-XIX), Department of Physical Geography, University of Barcelona, manuscript.īarriendos, M.: 1995a, ‘La climatologia histórica en el estudio de los riesgos climáticos. Aproximación a sus caracteristicas generales (ss. 31-58.īA Wasserwirtschaft (ed.): 1991, Ursachenanalyse der Hochwasser 1987-Ergebnisse der Untersuchungen, Mitteilungen des Bundesamtes für Wasserwirtschaft 4, Bern, 85 pp.īabió Wall, M.: 1990, Aproximación Etnográfica del Puerto y Rio de Sevilla en el Siglo XVI, Editorial Don Quijote, Sevilla, 254 pp.īarriendos, M.: 1994, El clima histórico de Catalunya. (ed.), Risques et aménagement dans les Pyrénées, GDR Isard, Toulouse, pp. Premiers résultats et problèmes d'interprétation’, in Métailié, J.-P. 221-235.Īntoine, J.-M., Desailly, B., and Métailié, J.-P.: 1991, ‘La chronologic des crues et des phénomènes torrentiels dans les Pyrénées (XVIIIe-XXe siècle). (ed.), Quaternary Climate in Western Mediterranean, Universidad Autonoma, Madrid, pp. A.: 1986, ‘Drought and rainy periods in the province of Zamora in the 17th, 18th and 19th centuries’, in Lopez Vera, F. ![]() Despite some limitations of documentary evidence, series of reconstructed historical floods are valuable sources of proxy data which can be utilized for the study of the flooding fluctuations in the pre-instrumental period.Īlvarez Vazquez, J. 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 (continuous heavy rains, sudden melting of thick snow cover, etc.). Changes in the flooding seasons in both halves of the century are not unambiguous. On the other hand, Italian and Catalonian rivers, in part, had a higher occurrence of floods during the first half of the century. Prevalence in flood occurrence during the second half of the sixteenth century in comparison to the first half is typical for central European and Andalusian rivers (mainly in the 1560s and 1590s) and agrees with the evolution of precipitation patterns. Different examples of modifications of the run-off process due to anthropogenic activity are discussed. The basic topographical and hydrological characteristics of the rivers investigated as well as the synoptic causes of their flooding during the instrumental period are presented. The severity and frequency of sixteenth-century floods of the Rhine, the Main, the middle and upper Elbe with its tributaries, rivers of northern and central Italy, the Garonne and rivers in Catalonia and Andalusia are analyzed using documentary evidence. ![]()
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