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Gäste schätzen die Erholung mit Lifestyle in relaxter Atmosphäre. Zeitraffer Heringsdorf-Bansin Mittags. Sie betreiben für ihren Ort oder ihr Unternehmen eine eigene Kamera, die Livebilder in hoher Auflösung zur Verfügung stellt? Webcam Wiek Rügen - Hafen. Impressum Datenschutz. Die beliebtesten Ferienorte an der Ostsee: Auf Ostsee24 Josephine Jobert Sie nicht nur zahlreiche Informationen zu einzelnen Ferienorten an der Ostseeküste, sondern auch die schönsten Ferienwohnungen. Le lingue Loch Auf Englisch in Italian. The Suebi eventually migrated southwest to temporarily reside in the Rhineland area of modern Germany, where their name survives in the historic region known as Swabia. See also: List of rivers of the Baltic Sea. Das Wetter im Zeitraffer. The Kattegat and the southwestern Baltic Sea are well oxygenated and have a rich biology. Alle Zeitrafferaufnahmen. For the first time ever, all the sources of pollution around an entire sea were made subject to a single convention, signed in by the then seven Baltic coastal states.Ostsee Tv Live - Live Webcam Bootshafen Kühlungsborn
Wir und unsere Partner verarbeiten personenbezogene Daten wie z. Es wurden HD Live Webcams in gefunden. IP- und Browserinformationen für folgende Zwecke:. Grömitz — Strand Grömitz: Seebrücke. Die Liste aller Partner kannst Du hier verwalten. Es wurden Star Crossed Trailer German Live Webcams in gefunden. Stream Chip Kiel, Holtenau, Schleuse. Bei schönem Wetter sieht man Menschen beim Schwimmen und Sonnenbaden. Sie ragt m in die Ostsee hinein. Sankt Peter-Ording. Die Livecam befindet sich auf der Konzertmuschel direkt an der Strandpromenade und schwenkt über die Ostsee zur Seebrücke Heringsdorf - mit Metern die längste Seebrücke in Kontinentaleuropa.Bitte beachte, dass auf Basis Deiner Einstellungen womöglich nicht mehr alle Funktionen der Seite zur Verfügung stehen.
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The sinking of the Wilhelm Gustloff remains the worst maritime disaster in history, killing very roughly 9, people.
In , a Russian group of scientists found over five thousand airplane wrecks, sunken warships, and other material, mainly from World War II, on the bottom of the sea.
Since the end of World War II , various nations, including the Soviet Union, the United Kingdom and the United States have disposed of chemical weapons in the Baltic Sea, raising concerns of environmental contamination.
Government refuses to disclose the exact coordinates of the wreck sites. Deteriorating bottles leak mustard gas and other substances, thus slowly poisoning a substantial part of the Baltic Sea.
After , the German population was expelled from all areas east of the Oder-Neisse line , making room for new Polish and Russian settlement.
Poland gained most of the southern shore. The Baltic states on the eastern shore were annexed by the Soviet Union. Neutral Sweden developed incident weapons to defend its territorial waters after the Swedish submarine incidents.
It ended only after the collapse of the Communist regimes in Central and Eastern Europe in the late s. Winter storms begin arriving in the region during October.
Older, wood-based shipwrecks such as the Vasa tend to remain well-preserved, as the Baltic's cold and brackish water does not suit the shipworm.
Storm surge floodings are generally taken to occur when the water level is more than one metre above normal. In Warnemünde about floods occurred from to , an average of just over two per year.
Historic flood events were the All Saints' Flood of and other floods in the years , , , , and Little is known of their extent.
The highest was the flood of when the water was an average of 2. In the last very heavy floods the average water levels reached 1. The Baltic Sea is one of the largest brackish inland seas by area, and occupies a basin a zungenbecken formed by glacial erosion during the last few ice ages.
The westernmost part of the Baltic Sea is the Bay of Kiel. The water temperature of the Baltic Sea varies significantly depending on exact location, season and depth.
In the deep of these basins the temperature variations are smaller. The ice-covered area during such a typical winter includes the Gulf of Bothnia , the Gulf of Finland , the Gulf of Riga , the archipelago west of Estonia, the Stockholm archipelago , and the Archipelago Sea southwest of Finland.
The remainder of the Baltic does not freeze during a normal winter, except sheltered bays and shallow lagoons such as the Curonian Lagoon.
The thickness decreases farther south. Freezing begins in the northern extremities of the Gulf of Bothnia typically in the middle of November, reaching the open waters of the Bothnian Bay in early January.
The Bothnian Sea , the basin south of Kvarken , freezes on average in late February. In , the Gulf of Finland was completely frozen on 15 February.
The ice extent depends on whether the winter is mild, moderate, or severe. In severe winters ice can form around southern Sweden and even in the Danish straits.
According to the 18th-century natural historian William Derham , during the severe winters of and , the ice cover reached as far as the Danish straits.
This description meant that the whole of the Baltic Sea was covered with ice. Since , the Baltic Sea has frozen over entirely 20 times, most recently in early , which was the most severe winter in Scandinavia since This was brought about by a stagnant high-pressure area that lingered over central and northern Scandinavia from around 10 to 24 February.
After this, strong southern winds pushed the ice further into the north, and much of the waters north of Gotland were again free of ice, which had then packed against the shores of southern Finland.
In recent years before , the Bothnian Bay and the Bothnian Sea were frozen with solid ice near the Baltic coast and dense floating ice far from it.
In , almost no ice formed except for a short period in March. During winter, fast ice , which is attached to the shoreline, develops first, rendering ports unusable without the services of icebreakers.
Level ice , ice sludge , pancake ice , and rafter ice form in the more open regions. Offshore of the landfast ice, the ice remains very dynamic all year, and it is relatively easily moved around by winds and therefore forms pack ice , made up of large piles and ridges pushed against the landfast ice and shores.
In spring, the Gulf of Finland and the Gulf of Bothnia normally thaw in late April, with some ice ridges persisting until May in the eastern extremities of the Gulf of Finland.
In the northernmost reaches of the Bothnian Bay, ice usually stays until late May; by early June it is practically always gone.
However, in the famine year of remnants of ice were observed as late as 17 July near Uddskär. Drift ice was also observed on 11 May The ice cover is the main habitat for two large mammals, the grey seal Halichoerus grypus and the Baltic ringed seal Pusa hispida botnica , both of which feed underneath the ice and breed on its surface.
Of these two seals, only the Baltic ringed seal suffers when there is not adequate ice in the Baltic Sea, as it feeds its young only while on ice.
The grey seal is adapted to reproducing also with no ice in the sea. The sea ice also harbors several species of algae that live in the bottom and inside unfrozen brine pockets in the ice.
Due to the often fluctuating winter temperatures between above and below freezing, the saltwater ice of the Baltic Sea can be treacherous and hazardous to walk on, in particular in comparison to the more stable fresh water-ice sheets in the interior lakes.
The Baltic Sea flows out through the Danish straits ; however, the flow is complex. The general circulation is anti-clockwise: northwards along its eastern boundary, and south along with the western one.
The difference between the outflow and the inflow comes entirely from fresh water. Additional fresh water comes from the difference of precipitation less evaporation, which is positive.
An important source of salty water is infrequent inflows of North Sea water into the Baltic. Such inflows are important to the Baltic ecosystem because of the oxygen they transport into the Baltic deeps, used to happen regularly until the s.
In recent decades they have become less frequent. The latest four occurred in , , , and suggesting a new inter-inflow period of about ten years.
The water level is generally far more dependent on the regional wind situation than on tidal effects. However, tidal currents occur in narrow passages in the western parts of the Baltic Sea.
The significant wave height is generally much lower than that of the North Sea. Quite violent, sudden storms sweep the surface ten or more times a year, due to large transient temperature differences and a long reach of the wind.
Seasonal winds also cause small changes in sea level, of the order of 0. The Baltic Sea is the world's largest inland brackish sea.
The Caspian Sea is larger in water volume, but—despite its name—it is a lake rather than a sea. The Baltic Sea's salinity is much lower than that of ocean water which averages 3.
The open surface waters of the Baltic Sea "proper" generally have a salinity of 0. The flow of freshwater into the sea from approximately two hundred rivers and the introduction of salt from the southwest builds up a gradient of salinity in the Baltic Sea.
The highest surface salinities, generally 0. It gradually falls further east and north, reaching the lowest in the Bothnian Bay at around 0.
As saltwater is denser than freshwater, the bottom of the Baltic Sea is saltier than the surface. This creates a vertical stratification of the water column, a halocline , that represents a barrier to the exchange of oxygen and nutrients, and fosters completely separate maritime environments.
Overall it follows the same southwest to east and north pattern as the surface. In contrast, the salinity of the Danish straits , which connect the Baltic Sea and Kattegat, tends to be significantly higher, but with major variations from year to year.
For example, the surface and bottom salinity in the Great Belt is typically around 2. From to inflows occurred on average six to seven times per decade.
Since it has been much less frequent, although a very large inflow occurred in The rating of mean discharges differs from the ranking of hydrological lengths from the most distant source to the sea and the rating of the nominal lengths.
Göta älv , a tributary of the Kattegat , is not listed, as due to the northward upper low-salinity-flow in the sea, its water hardly reaches the Baltic proper:.
Countries lands in the outer drainage basin :. The Baltic Sea drainage basin is roughly four times the surface area of the sea itself.
Most of the latter are in the Gulfs of Bothnia and Finland. The rest of the land is heavily populated. Geological surveys show that before the Pleistocene , instead of the Baltic Sea, there was a wide plain around a great river that paleontologists call the Eridanos.
Several Pleistocene glacial episodes scooped out the river bed into the sea basin. Instead of a true sea, the Baltic can even today also be understood as the common estuary of all rivers flowing into it.
From that time the waters underwent a geologic history summarized under the names listed below. Many of the stages are named after marine animals e.
The factors that determined the sea's characteristics were the submergence or emergence of the region due to the weight of ice and subsequent isostatic readjustment, and the connecting channels it found to the North Sea - Atlantic , either through the straits of Denmark or at what are now the large lakes of Sweden , and the White Sea - Arctic Sea.
The land is still emerging isostatically from its depressed state, which was caused by the weight of ice during the last glaciation.
The phenomenon is known as post-glacial rebound. Consequently, the surface area and the depth of the sea are diminishing. The uplift is about eight millimeters per year on the Finnish coast of the northernmost Gulf of Bothnia.
In the area, the former seabed is only gently sloping, leading to large areas of land being reclaimed in what are, geologically speaking, relatively short periods decades and centuries.
The "Baltic Sea anomaly" refers to interpretations of an indistinct sonar image taken by Swedish salvage divers on the floor of the northern Baltic Sea in June The treasure hunters suggested the image showed an object with unusual features of seemingly extraordinary origin.
Speculation published in tabloid newspapers claimed that the object was a sunken UFO. A consensus of experts and scientists say that the image most likely shows a natural geological formation.
The fauna of the Baltic Sea is a mixture of marine and freshwater species. Among marine fishes are Atlantic cod , Atlantic herring , European hake , European plaice , European flounder , shorthorn sculpin and turbot , and examples of freshwater species include European perch , northern pike , whitefish and common roach.
Freshwater species may occur at outflows of rivers or streams in all coastal sections of the Baltic Sea. Otherwise marine species dominate in most sections of the Baltic, at least as far north as Gävle , where less than one-tenth are freshwater species.
Further north the pattern is inverted. In the Bothnian Bay, roughly two-thirds of the species are freshwater.
In the far north of this bay, saltwater species are almost entirely absent. Their range limit is west of Bornholm, meaning that they are absent from the vast majority of the Baltic Sea.
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