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Lake Neusiedl

Steppe lake in Central Europe

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  • 4 chapters

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Through Drainage basin, UNESCO and Common Era

The surrounding landscape has been occupied since about 6000 BC, and the towns and villages around the lake have been trading and meeting points for local people and wider cultures for centuries. Given its cultural importance and the often handed-down, rustic architecture of the villages, Lake Neusiedl and environs is inscribed on the UNESCO World Heritage List since 2001.

Water level fluctuations

In the past, rainfall caused significant floods (which in 1768 enlarged the lake to its greatest known size of 515 km2 [199 sq mi]) whereas aridity led to shrinkage. Yet as a function of its water table, frequent changes resulted from weather changes.

Stratigraphy shows that the lake bed has totally dried up at least 100 times since its formation in 18,000–14,000 BCE. The lake's complete disappearances - particularly 1740–1742, 1811–1813, and most recently in 1866, when the private diary of a local, Gottlieb Wenzel, noted that he crossed its bed on 4 June without soiling his boots - were greatly documented. Parts of the lake bed were claimed for agriculture; wheat and turnips were being planted. However, in 1871 the lake began to return and by the spring of 1876 it had already reassumed its usual size. The last (brief and partial) vanishing took place during the summer of 1949 when the northern part of the lake bed (to the approximate latitude of Podersdorf) fell dry for a few weeks. Each time the drying-up of the lake bed caused major environmental disruptions:

  • The humidifying and heatwave counteraction of the large water body fell absent
  • Winds blew large amounts of salty dust into the surrounding villages.

On earlier occasions the lake was sometimes referred to as a "swamp", suggesting a very low water level with an expansion of reeds throughout the lake bed. Two records dated to 1318 and 1324, respectively mention a "river", implying that at this time the lake might have been reduced to a narrow north-to-south slightly flowing body of water.

Today bank overflow is stopped by an artificial outflow, the Einserkanal, and a sluice on Hungarian territory near Fertőújlak, and bilateral issues are dealt with by the Austro-Hungarian water commission which was established in 1956. However, comparatively minor fluctuations continue to occur. In 1965 the lake gained 100 million cubic metres (3.5 billion cubic feet) of water within one month, raising its level by 35 cm (14 inches). A falling away by 30 cm (12 inches) within one year took place amid the drought of 2003. Both events are deemed within normal range, as noted publicly by the local planning law authorities. Evaporation can be exacerbated or compensated by the effects of air pressure, alone, giving a range of 75 cm (30 inches). The lake is sensitive to changes in its equilibrium, as recent climate change scenario simulations have shown.

Before the regulation works of the 19th century, the lake reached in the southeast to the marshlands of the Hanság (German: Waasen) which have been increasingly drained and claimed for agriculture from the 16th century onward. Originally, the lake was thus closely connected to the Danube and the Rába river systems.

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