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   » » Wiki: Kattegat
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The Kattegat (; ; ) is a sea area bounded by the peninsula of in the west, the islands of and the to the south and the Swedish provinces of Bohuslän, Västergötland, and in in the east. The Baltic Sea drains into the Kattegat through the . The sea area is a continuation of the and may be seen as a bay of the and North Atlantic Ocean, though this is not the case in traditional usage.

The Kattegat is a rather shallow sea and can be dangerous to navigate due to many sandy, stony reefs and the tricky shifting currents. In modern times, artificial seabed channels have been dug, many reefs have been either by sand pumping or boulder clearance, Artificial Reefs and a well-developed network has been installed to protect the heavy international traffic on this small sea.

There are several large cities and major ports on the Kattegat, including, in descending size, , , , , and .


Geography
According to the definition established in a 1932 convention signed by Denmark, and Sweden (registered in the League of Nations 1933–1934), the northern boundary between the Kattegat and Skagerrak is at the northernmost point of on Jutland and the southern boundary towards Øresund is at the tip of Kullen Peninsula in Scania. Convention No 3210. League of Nations Treaty Series 139, 1933–1934. Retrieved 27 December 2012.

Major that drain into the Kattegat are the rivers of Göta älv at , together with the Lagan, Nissan, Ätran and in the province of on the Swedish side, and the Danish river of Gudenå in Jutland.

The main islands of the Kattegat are Samsø, Læsø and Anholt; due to their relatively dry climate, the last two are, perceived to belong to "the Danish desert belt".

A number of noteworthy coastal areas abut the Kattegat, including the Kullaberg Nature Reserve in Scania, which contains a number of and a scenic , the town of Mölle, which has a picturesque harbour and views into the Kullaberg, and Skagen at the northern tip of Denmark.

Since the 1950s, a bridge project usually referred to as Kattegatbroen (the ) connecting Jutland and Zealand across the Kattegat has been considered. Since the late 2000s, the project has seen a renewed interest from several influential politicians in Denmark. The bridge is usually envisioned as connecting Hov (a village south of in the Aarhus area) with Samsø and .


Extent
The International Hydrographic Organization defines the limits of the "Kattegat, Sound and Belts" (that is, the Kattegat, Øresund, , and ) as follows:


Etymology
According to Den Store Danske Encyklopædi and , the name is from the words katte 'cat's' and gat 'gate, passage'. It derives from late navigation jargon, in which captains of the trading fleets would compare the to a passage so tight that even a cat would have difficulty squeezing its way through, owing to the many and shoals. Den Store Danske Encyklopædi (2004), CD-ROM edition, Copenhagen: Gyldendal, entry Kattegat. Nudansk Ordbog (1993), 15th edition, 2nd reprint, Copenhagen: Politikens Forlag, entry Kattegat. At one point, the passable waters were a mere wide. The name of the street has a comparable etymological meaning, namely 'narrow passage', .

An archaic name for both the and Kattegat was the Norwegian Sea or Jutland Sea (Knýtlinga saga mentions the name Jótlandshaf). Its ancient name was Sinus Codanus.


History
Controlling and having access to the Kattegat have been important throughout the history of international seafaring. Until the completion of the in 1784, the Kattegat was the only sea route into and out of the Baltic region.

Beginning in 1429 in the , the Danish royal family – and later the state of Denmark – prospered greatly from the , a toll charged for passage through the Øresund, while sheltered and repaired ships and provided trade opportunities and protection from . The dues were eventually lifted, in 1857.


Biology
The in the Kattegat has a pronounced two-layer structure. The upper layer's salinity is between 18‰ and 26‰, while that of the lower layer (separated by a strong at around ) has a salinity between 32‰ and 34‰. The lower layer consists of inflowing seawater from the Skagerrak, with a salinity on par with most other coastal seawaters, while the upper layer, consisting of inflowing seawater from the Baltic Sea, has a much lower salinity, comparable to , but still a great deal higher than the rest of the Baltic. These two opposing flows transport a net surplus of of seawater from the Baltic to the Skagerrak every year. During strong winds, the Kattegat's layers are completely mixed in places such as the , making the overall salinity highly variable. This leads to some distinctive conditions for in the area.
(2025). 9783540797036, Springer-Praxis. .

, known locally as bubbling reefs (), can be found in the northern Kattegat. Unlike those in most other places (including the North Sea and Skagerrak), the Kattegat's cold seeps are at relatively shallow depths, generally from below the surface. The seeps rely on methane deposited during the period and during calm weather the bubbles can sometimes be seen on the surface of the water. Carbonate cementation and form slaps or pillars up to tall and support a rich . Due to their distinct properties, the Kattegat bubbling reefs are under protection and are recognised by the (EU) as a Natura 2000 habitat (type 1180).


Ecological collapse
The Kattegat, characterised by widespread anoxia, was one of the first marine dead zones to be noted in the 1970s, when scientists began to study the effects of heavy industry on the natural world.
(2025). 9781285402222, Brooks/Cole. .
Since then, research has leant much insight into processes like , and how to deal with it. Since the first Action Plan for the Aquatic Environment in 1985, Denmark and the EU have begun costly, far-reaching domestic projects to stop, repair and prevent these environmentally destructive and economically damaging processes
(1996). 9780875902661
and are now busy implementing the fourth Action Plan. The action plans sum up a broad range of initiatives and include the so-called Nitrate Directives. Implementation of the Nitrates directive in Denmark Danish Ministry of the Environment The action plans have generally been viewed as a success, although the work is not finished and not all goals have been met yet.


Protections and regulation
Due to its very heavy sea traffic and many large coastal settlements, the Kattegat has been designated as a Sulphur Emission Control Area as part of the Baltic Sea since 2006. As from 1 January 2016 the benchmark for sulphur in fuels was lowered to 0.1%.

Several large areas of the Kattegat are designated under Natura 2000 and various bird protections such as the Ramsar Convention. The remaining larger shallow reefs are among the protections, as they are important spawning and feeding grounds for fish and marine mammals and support a thriving but threatened . Protected areas include:

Denmark

  • The Bay of Aalborg, comprising a shallow sea area.
  • on Læsø and the stony south of the island.
  • Anholt and the sea north of the island.

Sweden

  • The Nordre älv north of Gothenburg. An important spot for migratory birds and fish.
  • The Vrångö archipelago (Swedish: Vrångöskärgården), part of the Archipelago of Gothenburg. An important reproduction area for seabirds and seals.
  • . A shallow water fjord between Gothenburg and , including important .
  • Kullaberg Nature Reserve

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