“St. Mary Magdalene's flood”的意思、由来-开放百科全书

St. Mary Magdalene's flood (German: Magdalenenhochwasser) was the largest-recorded flood in central Europe^[1] with water levels exceeding those of the 2002 European floods. It occurred in July 1342 on and around the feast day of St. Mary Magdalene, 22 July.

Following the passage of a Genoa low the rivers Rhine, Moselle, Main, Danube, Weser, Werra, Unstrut, Elbe, Vltava and their tributaries inundated large areas. Many towns such as Cologne, Mainz, Frankfurt am Main, Würzburg, Regensburg, Passau and Vienna were seriously damaged. Even the river Eider north of Hamburg flooded the surrounding land. The affected area extended to Carinthia and northern Italy.

It appears that after a prolonged hot and dry period continuous rainfalls occurred which lasted several consecutive days and amounted to more than half of the mean yearly precipitation. Since the dry soil was unable to absorb such amounts of water, the surface runoff washed away large areas of fertile soil and caused huge inundations destroying houses, mills and bridges. In Würzburg, the then famous Steinerne Brücke (Stone Bridge) was taken away and in Cologne it is said that a rowing boat could pass over the city's fortifications. The overall number of casualties is not known, but it is believed that alone in the Danube area 6,000 people were killed. The results of the erosion can still be noticed today. The volume of the eroded soil during this short incident (a few days) is determined to be more than 13 billion metric tons,^[2] a volume that is washed away under normal climate conditions over a period of 2,000 years.^[3]

It is assumed that the loss of fertile soil led to a serious drop in agricultural production. In addition, the following summers were wet and cold, so that the population suffered from widespread famine. Whether the spreading of the Black Death between 1348 and 1350 killing at least a third of the population in central Europe was facilitated by the weakened condition of the population is a matter of discussion.

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1. ^Without taking the storm surges on the North Sea coasts into account
2. ^{{Citation | last =Bork | first =Hans-Rudolf | author-link =Hans-Rudolf Bork | last2 =Piorr | first2 =Hans-Peter | author2-link =Hans-Peter Piorr | title =Innovative Ansätze zum Schutz der Natur: Visionen für die Zukunft | editor-last =Erdmann | editor-first =Karl-Heinz | editor2-last =Mager | editor2-first =Thomas J. | place = | publisher =Springer | year =2000 | chapter =Integrierte Konzepte zum Schutz und zur dauerhaft-naturverträglichen Entwicklung mitteleuropäischer Landschaften – Chancen und Risiken, dargestellt am Beispiel des Boden- und Gewässerschutzes | pages =71–72 | language =de | isbn =978-3540666677 }}
3. ^{{Citation| last =| first =| author-link =| last2 =| first2 =| author2-link =| title =Das verflixte "Genua-Tief"| publisher =Neue Zürcher Zeitung| date =2008-08-25| year =| url =http://www.nzz.ch/2005/08/25/il/articleD31CG.html| access-date =2016-02-12| deadurl =yes| archiveurl =https://web.archive.org/web/20111230134322/http://www.nzz.ch/2005/08/25/il/articleD31CG.html| archivedate =2011-12-30| df =}}

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