Divisions Lake Constance is located in the foothills of the
Alps. The shore length of both main lakes is long. Of this, are located in Germany (
Baden-Württemberg ,
Bavaria ), run through Austria and through Switzerland. If the upper and lower lakes are combined, Lake Constance has a total area of , the third largest lake in
Central Europe by area after
Lake Balaton () and
Lake Geneva (). It is also the second largest by water volume () after Lake Geneva () and extends for over between
Bregenz and
Stein am Rhein. Its
catchment area is around , and reaching as far south as
Lago di Lei in Italy. The area of the
Obersee, or Upper Lake, is . It extends from Bregenz to
Bodman-Ludwigshafen for over and is wide between
Friedrichshafen and
Romanshorn. At its deepest point between
Fischbach and
Uttwil, it is deep. in 2007 The three small bays on the
Vorarlberg shore have their own names: the Bay of Bregenz, off
Hard and
Fußach is the Bay of Fussach and, west of that is the Wetterwinkel. Farther west, now in Switzerland, is the Bay of Rorschach. To the north, on the Bavarian side, is the Bay of Reutin. The railway embankment from the mainland to the island of Lindau and the motorway bridge over the lake border the so-called Little Lake (
Kleiner See), which is located between the Lindau village of Aeschach and the island. The northwestern, finger-shaped arm of the Obersee is called Überlinger See (or Überlingersee in
Swiss Standard German), or
Lake Überlingen. It is sometimes regarded as a separate lake, the boundary between Lake Überlingen and the rest of the Upper Lake runs approximately along the line between the southeast tip of Bodanrück (the
Hörnle, which belongs to the town of Konstanz) and Meersburg. The
Constance Hopper lies between the German and Swiss shores east of
Konstanz. The Obersee and Untersee are connected by the
Seerhein. The
Untersee, or Lower Lake, which is separated from the Obersee and from its north-west arm, the Überlinger See, by the large peninsula of
Bodanrück, has an area of . It is strongly characterised and divided into different areas by
end moraines, various
glacial snouts and
medial moraines. These various areas of the lake have their own names. North of
Reichenau Island is the
Gnadensee. West of the island of Reichenau, between the peninsula of
Höri and the peninsula of
Mettnau is the Zeller See (or Zellersee in Swiss Standard German), or
Lake Zell. North of the peninsula and swamp land Mettnau lies the lake part Markelfinger Winkel. The
drumlins of the southern Bodanrück continue along the bed of these northern parts of the lake. South of the Reichenau, from
Gottlieben to
Eschenz, stretches the
Rheinsee (lit.: "Rhine Lake") with strong Rhine currents in places. Previously this lake part was named Lake Bernang after the village of
Berlingen. On most of the maps the name of the
Rheinsee is not shown, because this place is best suited for the name of the Untersee.
Emergence and future The present-day shape of Lake Constance has resulted from the combination of several factors: • The
tectonic Lake Constance Basin between the Alps and the Jura was created in the
Jurassic and
Tertiary periods. • The current
Alpine Rhine was initially a tributary of the Danube. • Over time, the basin was
captured by the
High Rhine as a result of
headward erosion (
fluvial erosion). • The capture was not always only along the present Rhine valley;
Lake Überlingen marks part of an older valley course. • The river valleys were deepened during several
cold periods by the
Rhine Glacier from the valley of the Alpine Rhine (
glacial erosion). • Behind the present impressive traces of the
Würm Ice Age, the effects of older cold periods can no longer be explored in any detail. Lake Constance now represents, above all, a
zungenbecken or
glacial lake of the Würm Glaciation. • During a later phase of the ice age, only the Obersee was glaciated. As the glacier retreated further, the
glacial meltwaters flowed out of the emerging Überlingen See through the older more northerly valley into the present High Rhine valley. • Due to the advancing headward erosion, the present course of the High Rhine was finally (again) reconnected to Lake Constance. Like any glacial lake, Lake Constance will also silt up by
sedimentation. This process can best be observed at the mouths of the larger rivers, especially that of the Alpine Rhine. The
silting up process is accelerated by ever-increasing erosion by the Rhine and the associated reduction in the level of the lake.
Tributaries The main tributary of Lake Constance is the
Alpine Rhine. The Alpine Rhine and the
Seerhein do not mix greatly with the waters of the lake and flow through the lakes along courses that change relatively little. There are also numerous smaller tributaries (236 in all). The most important tributaries of the Obersee are (counterclockwise) the
Dornbirner Ach,
Bregenzer Ach,
Leiblach,
Argen,
Schussen,
Rotach,
Brunnisach,
Seefelder Aach,
Stockacher Aach,
Salmsacher Aach, the
Aach near Arbon,
Steinach,
Goldach and the
Old Rhine. The outflow of the Obersee is the
Seerhein, which in turn is the main tributary of the Untersee. The most important tributary of the Untersee is the
Radolfzeller Aach. The source of the Radolfzeller Aach is the
Aachtopf, a
karst spring whose waters mostly derive from the
Danube Sinkhole. Therefore, the
Danube is indirectly also a tributary of the Rhine. Empty cells mean there is no data in the publications. --> Because the Alpine Rhine brings with it
drift from the mountains and deposits this material as
sediment, the Bay of Bregenz will silt up in a few centuries time. The silting up of the entire Lake Constance is estimated to take another ten to twenty thousand years.
Outflows, evaporation, water extraction The outflow of the Untersee is the
High Rhine with the
Rhine Falls at
Schaffhausen. Both the average precipitation of 0.45 km3/a and evaporation which averages 0.29 km3/a cause a net change in the level of Lake Constance that is less when compared to the influence of the inflows and outflows.
mini|Das 75-jährige österreichische Flaggschiff Austria (Schiff, 1939)|Austria im Hafen von Bregenz vor dem Pfänder. •
Bregenz: 1842/46 Bau einer hölzernen Hafenanlage für sechs Dampfschiffe; 1850 Ersatz durch eine Steinmole; 1872 Eisenbahnanschluss; 1884 Gründung der österreichischen Bodenseeflotte mit Heimathafen Bregenz; ab 1881 Hafenerweiterung mit
Trockendock (bis 1940) und Trajektverbindungen nach Romanshorn, Konstanz und Friedrichshafen (bis 1913/17). Der Hafen besteht seitdem aus einem „großen Molo“ als Wellenbrecher, einem mittleren „Personenmolo“ mit Hafengebäude und Liegeplätze für drei Schiffe im Einsatz sowie einem „Reservemolo“ für Schiffe außer Betrieb. Zwischen diesen beiden wurde 1977 ein eiserner Steg mit Tankstelle errichtet. Bei der Sanierung 1996 wurden Liegeplätze für Privatboote geschaffen. •
Rorschach: 1840 neue Hafenmole für den immer noch zu kleinen Hafen, deshalb 1862 Erweiterung zur heutigen Größe; 1856 unmittelbarer Eisenbahnanschluss; Heimathafen der drei kleinen
SBS-Schiffe des ehemaligen
Schifffahrtsbetriebs Rorschach. •
Romanshorn: Aus dem kleinen Hafen (1844) des Fischerdorfes entstand bis 1870 der flächenmäßig größte Bodenseehafen mit Gleisanschluss (1855) und Bahnhof direkt am Hafen und Trajektverbindungen nach Deutschland. Als Verkehrsknotenpunkt wurde der Heimathafen der vier großen SBS-Schiffe so bedeutsam, dass sich der Ort um den Hafen entwickelte. Die Trajekte wurden durch die Autofährlinie Friedrichshafen-Romanshorn abgelöst. Die leistungsfähige Werft ist heute die einzige dieser Art am Bodensee. •
Unteruhldingen: Der Ausflugs- und ehemalige Fährhafen befindet sich zwischen der Marina und dem ehemaligen Bahnhof. Die
Bodensee-Schiffsbetriebe bieten Verbindungen nach Konstanz, Mainau, Überlingen, Meersburg, Daisendorf und Rorschach an.--> Additionally,
car ferries link Romanshorn to Friedrichshafen, and Konstanz to Meersburg. It docks at the harbours of
Kreuzlingen, Konstanz,
Gottlieben,
Ermatingen,
Reichenau,
Mannenbach,
Berlingen,
Gaienhofen,
Steckborn,
Hemmenhofen, Wangen,
Mammern,
Öhningen,
Stein am Rhein,
Diessenhofen,
Büsingen and Schaffhausen.
Radolfzell and
Iznang are also linked by a boat line over the Lower Lake (to Konstanz).
Rail (S1) trainset on the
Vorarlberg Railway line A network of several
railway lines surrounds the lake. The lines are operated by regional train services (
S-Bahn,
RegioExpress,
Regional-Express) spreading over four countries (
Austria,
Germany,
Liechtenstein,
Switzerland). In Switzerland, they belong to
S-Bahn St. Gallen and trains are operated by
THURBO (
Swiss Federal Railways, SBB),
Südostbahn (SOB) and
Appenzell Railways (AB). The so-called
belt railway () along the northern shore is operated by
DB Regio and
SBB GmbH. In Austria and Liechtenstein, train services are operated by
Austrian Federal Railways (ÖBB) for the
Vorarlberg S-Bahn. Regional train services around Lake Constance are marketed as
Bodensee S-Bahn.
Railway stations close to harbours are, among others: , , , , , , and . Long-distance trains (
RJ/RJX,
EC/ECE,
IC (DB)/
IC (SBB),
IR,
IRE) link larger lakeside railway stations (e.g., , , , , ) with major cities.
Air Two
airports are located near the lake's shores:
Friedrichshafen Airport (Germany) and
St. Gallen–Altenrhein Airport (Switzerland).
Zeppelin NT offers touristic
zeppelin flights around Lake Constance departing from Friedrichshafen Airport.
Climate in Lindau The climate of the Lake Constance area is characterised by mild temperatures with moderate gradients, thanks to the balancing and retarding effect of the large body of water. It has a
subtropical microclimate, which allows the cultivation of some exotic fruits and trees. Constance counts 2069 sunshine hours a year and is therefore considered one of the sunniest cities in Germany. Winters are generally short and mild, although night temperatures can fall under 0°C, especially from December to February. Typically day temperatures range between +5 and +12°C, while nights with +1 to +8°C on average stay cold, though mostly without long and severe frosts. The
Föhn, a warm wind from the
Mediterranean Sea, that regularly blows through the Alps, can cause temperatures between 15 and 20°C with sunshine for several days, while on the other hand fog creates a few cold days between 1 and 5°C each year. Generally, Lake Constance is affected more by fog than neighboring regions more inland. Spring goes from March to May and is usually sunny, with day temperatures between 15 and 22°C but still relatively cold water. This is also resulting in still cold night temperatures that range between 4°C in March and 12°C in May only. As the lake temperature heats up by the increasing warm days, the nights are also becoming milder, though moderated a little bit by the height and lake. This results in average morning lows of 16-18°C during the high summer months. Lake Constance counts one of the highest amount of
tropical nights in Germany (lowest temperature at 20°C or more). The days in Summers (June-September) are warm to hot with day temperatures of 26-33°C on average, decreasing to around 20°C until the end of September. Humidity levels raise noticeable and temperatures often move up to 35°C between June and August. This increases the
heat index, causing Lake Constance to have a stressful climate. The region receives most of its sunny days during high summer. In the recent years, in 2018 and 2022, the water levels fall to new record lows due to weeks without significant rain. On the other hand, the closeness to the Alps can cause thunderstorms in the evenings that sometimes occur out of nowhere. While the official bathing season ends in September, the average lake temperature stays around 20°C until October. Autumn is generally the time when Lake Constance starts to experience more foggy mornings again, but the day temperatures still range between 21 in the beginning and 10-12°C at the end of the season. Night temperatures fall from 13°C in September to an average of 5°C in November. Lake Constance is one of the best known wine growing regions in Germany and experiences several outdoor events during harvest time in autumn. Lake Constance is also considered to be a risky and challenging lake for water sports because of the danger of gusty winds which can whip up waves as the weather changes suddenly. The most dangerous wind is the föhn, a warm down-slope wind from the Alps, which spreads out across the water, especially through the
Alpine Rhine Valley and can generate waves several metres high. Similarly dangerous for those unfamiliar with the area, are the sudden stormy gusts of wind during summer thunderstorms. They constantly claim victims from the water sports fraternity. During a thunderstorm in July 2006, waves reached heights of up to 3.50 metres. For these reasons, there is a storm warning system in all three neighbouring countries. For
storm warning purposes, Lake Constance is divided into three warning regions (west, centre and east). Warnings can be issued for each region independently. A "high winds" warning will be issued when
squalls are expected of between 25 and 33
knots or registering
force 6 to 8 on the
Beaufort scale. A
gale warning announces the likelihood of gale-force winds, i.e. those at speeds as of 34 knots or more or force 8 on the Beaufort scale. In order to issue these warnings, orange-coloured flashing lights are installed around the lake, which flash at a frequency of 40 times per minute for high winds or 90 times per minute for gales. It can happen that, due to the differently regulated responsibilities and assessments, a gale warning is issued on the Swiss side of the Obersee, but not on the German or Austrian shores, and vice versa. Ships and ferries on Lake Constance indicate a gale warning by hoisting a
Sturmballon ("storm ball") up the mast.
Freeze over A one-hundred year event is the freezing over of Lake Constance, when the Lower Lake and the Upper Lake are completely frozen over so that people can safely cross the lake on foot. The last so-called
Seegfrörne (
Alemannic) event was in 1963. The following is a list of
years in which Lake Constance froze over partially or completely: • 875, 895 • 1074, 1076 • 1108 • 1217, 1227, 1277 • 1323, 1325, 1378, 1379, 1383 • 1409, 1431, 1435 (complete), 1460, 1465, 1470, 1479 • 1512, 1517, 1553, 1560 (complete), 1564, 1565, 1571, 1573 (complete) • 1684, 1695 (complete) • 1788, 1796 (complete) • 1830 (complete), 1880 (complete) • 1929, 1963 (complete) Certain parts of the lake freeze over more frequently, mainly due to their shallow depth of water and shelter, as is the case, for example, of the so-called
Markelfinger Winkel between the municipality of
Markelfingen and the
Mettnau peninsula.
Floods • A
100-year flood around June 1999 (
Pfingsthochwasser 1999) raised the level about 2 metres above normal, flooding harbors and many shoreline buildings and hotels. • In late August 2005, heavy rain raised the level by more than in a few days. The rains caused widespread flooding and washed out highways and railroads. • Frequent rainfall and snowmelt in the summer of 2024 raised water levels to above normal level.
International borders The lake lies where the countries of Austria, Germany, and Switzerland meet. Beyond areas less than deep, considered to be under the jurisdiction of the nearest country, there is no legally binding agreement as to where the borders lie between the three countries. However, Switzerland holds the view that the border runs through the middle of the lake, Austria is of the opinion that the contentious area belongs to all the states on its banks, which is known as a "
condominium", and Germany holds an ambiguous opinion. Legal questions pertaining to ship transport and fishing are regulated in separate treaties. Disputes occasionally arise. One concerns a
houseboat which was moored in two states (
ECJ c. 224/97 Erich Ciola); another concerns the rights to fish in the Bay of Bregenz. In relation to the latter, an Austrian family was of the opinion that it alone had the right to fish in broad portions of the bay. However, this was accepted neither by the Austrian courts nor by the organs and courts of the other states. == Ecology ==