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・ 2013 Federated Auto Parts 400
・ 2013 European Diving Championships – Men's 3 metre springboard
・ 2013 European Diving Championships – Men's 3 metre synchro springboard
・ 2013 European Diving Championships – Men's synchronized 10 metre platform
・ 2013 European Diving Championships – Team event
・ 2013 European Diving Championships – Women's 1 metre springboard
・ 2013 European Diving Championships – Women's 10 metre platform
・ 2013 European Diving Championships – Women's 3 metre springboard
・ 2013 European Diving Championships – Women's 3 metre synchro springboard
・ 2013 European Diving Championships – Women's synchronized 10 metre platform
・ 2013 European Dressage Championship
・ 2013 European Eventing Championship
・ 2013 European F3 Open season
・ 2013 European Fencing Championships
・ 2013 European Figure Skating Championships
2013 European floods
・ 2013 European Formula 3 season
・ 2013 European Individual Chess Championship
・ 2013 European Judo Championships
・ 2013 European Junior Badminton Championships
・ 2013 European Junior Cup season
・ 2013 European Junior Curling Challenge
・ 2013 European Junior Swimming Championships
・ 2013 European Karate Championships
・ 2013 European Kendo Championships
・ 2013 European Le Mans Series season
・ 2013 European Masters (curling)
・ 2013 European Mixed Curling Championship
・ 2013 European Modern Pentathlon Championships
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2013 European floods : ウィキペディア英語版
2013 European floods

Extreme flooding in Central Europe began after several days of heavy rain in late May and early June 2013. Flooding and damages primarily affected south and east German states (Thuringia, Saxony, Saxony-Anhalt, Lower Saxony, Bavaria and Baden-Württemberg), western regions of the Czech Republic (Bohemia), and Austria. In addition, Switzerland, Slovakia, Belarus, Poland, Hungary and Serbia (Vojvodina) were affected to a lesser extent. The flood crest progressed down the Elbe and Danube drainage basins and tributaries, leading to high water and flooding along their banks.
==Meteorological history==
The spring weather preceding the flooding had been wet in the region, and May 2013 had been one of the three wettest in the last 156 years in Austria, together with the years 1962 and 1965. Austria saw twice as much rainfall as average during the month, resulting in the ground in the region becoming saturated. Soils in Germany were showing record levels of moisture prior to the rains. The already saturated soils led to greater runoff when the rains began.
In last ten days of May a low pressure system named "Christoffer" swung up from the Mediterranean across the Black Sea then across Ukraine and Poland to Northern Germany, eventually bringing a very moist, and warm airmass to Central Europe from north-east. Late May saw a blocking high "Sabine" located over the Sole sea area to the west of the UK and France. This split the jet stream over Europe which maintained the weather pattern in Central Europe.
Spring and summer flooding in Central Europe is commonly associated with the so-called "Zugstrasse Vb" track of low pressure areas, which bring low pressure and moist air from the Mediterranean Sea over Central Europe, and have led to severe flooding in the affected region before. Though later analysis found this flooding did not fit into this type.
Low pressure areas "Frederik" and "Günther" formed over the northern Adriatic and tracked north towards central Europe. The high pressure "Sabine" and low pressure areas brought an airflow from the north across Germany, which brought the water-laden air from the north east. The air mass was pushed to the south west by the northerly flow, where it was lifted as it moved south from the North European Plain over the Thuringian Forest, Ore Mountains, and Bohemian Forest. The air was then lifted along the north side of the Alps in Austria as the air masses were pushed into the Alps by the northerly flow, which led to intense orographic precipitation. Heavy rain was reported in the Austrian states of Vorarlberg and Tyrol and the area of Salzburg, and to the mountains of Upper Austria and Lower Austria and Upper Styria in a short time.
On 30 May to 1 June, 150 to 200 mm of rain ( of rain) fell, in places reaching around 250 mm (), which in just a few days was the equivalent normally seen over two and a half months on average. The rainfall experienced in Austria has an expected return period of between 30 and 70 years. The bulk of the rain fell in only two days in Salzburg, Tyrol, and Vorarlberg, which is thought to have a return period of more than 100 years.
Following the intense rain, sporadic showers and rainfall continued to raise the risk of further flooding but no rainfall of the intensity as that seen on 31 May-2 June occurred. Some Flash flooding occurred in the Polish capital Warsaw on 9 June, as a result of thunderstorms.
The flood waters were expected to exceed the levels seen during the disastrous "once in a century" Central European floods of 2002 in some areas. In Bavaria and eastern Germany water levels significantly exceeded those of 2002 in many places on the Danube and Elbe. In Passau, at the confluence of the rivers Danube, Inn and Ilz, the highest water level since 1501 was recorded. In Dresden, by contrast, the old city centre was largely spared, unlike in 2002. Thanks to better flood control, fewer dykes on the upper reaches of the Elbe broke than in 2002, but this meant that the flood wave further downstream was all the higher. In Magdeburg, the floods reached a record level.〔

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