Lower Oder Plain
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Lower Oder Plain
Szczecin Lagoon ( pl, Zalew Szczeciński, german: Stettiner Haff, since 1945 sometimes also ''Oderhaff'' (Oder lagoon) or ''Pommersches Haff'' ( Pomeranian lagoon)) is a lagoon in the Oder estuary, shared by Germany and Poland. It is separated from the Pomeranian Bay of the Baltic Sea by the islands of Usedom and Wolin. The lagoon is subdivided into the ''Kleines Haff'' ( pl, Mały Zalew, "small lagoon") in the West and the ''Wielki Zalew'' (german: Großes Haff, "great lagoon") in the East. An ambiguous historical German name was ''Frisches Haff'', which later exclusively referred to the Vistula Lagoon. Geography From the South, the lagoon is fed by several arms of the Oder river and smaller rivers like Ziese, Peene, Zarow, Uecker, and Ina.Gerald Schernewski, ''Baltic coastal ecosystems: structure, function, and coastal zone management'', Springer, 2002, p.79, In the North, the lagoon is connected to the Baltic Sea's Bay of Pomerania with the three straits Peene ...
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West New Britain Province
West New Britain is a province of Papua New Guinea on the islands of New Britain. The provincial capital is Kimbe. The area of the province is 20,387 km² with a population of 264,264 as of the 2011 census. The province's only land border is with East New Britain. There are seven major tribes, the Nakanai, Bakovi, Kove, Unea, Maleu, Arowe, speaking about 25 languages. People from West New Britain are referred to as "Kombes" in Papua New Guinea, in metonymic reference to the significant Kove (or Kombe) people. The Kove people were reported on by the anthropologist Ann Chowning in ''National Geographic'' magazine during the 1960s. Within Papua New Guinea they are noted for their practice of superincision of the penis — circumcision is generally though inaccurately referred to among Papua New Guineans as "the Kombe cut" — but was formerly practiced in other northern coastal regions of New Guinea island and the New Guinea Islands. The predominant religious affiliation is Roma ...
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Peene
The Peene () is a river in Germany. Geography The Westpeene, with the Ostpeene as its longer tributary, and the Kleine Peene/Teterower Peene (with a ''Peene '' without specification (or ''Nordpeene'') as its smaller and shorter affluent) flows into Kummerower See (Lake Kummerow), and from there as Peene proper to Anklam and into the Oder Lagoon. The western branch of the Oder River, which separates the island of Usedom from the German mainland, is often also called Peene, but actually is considered a part of the Baltic Sea called the Peenestrom. It is one of three channels connecting the Oder Lagoon with the Bay of Pomerania of the Baltic Sea. (The other channels are the Świna and the Dziwna.) Ostpeene-30-04-2008-263.jpg, Ostpeene Teterow-stadtmuehle.jpg, Old watermill on Kleine Peene in Teterow Peene-in-Demmin-26-VIII-2007-07.jpg, Peene harbour in Demmin Peene bei Loitz.JPG, Peene river near Loitz Peene bei Jarmen.jpg, Peene river near Jarmen Anklam Peene Fussgängerbrüc ...
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Szczecin
Szczecin (, , german: Stettin ; sv, Stettin ; Latin: ''Sedinum'' or ''Stetinum'') is the capital and largest city of the West Pomeranian Voivodeship in northwestern Poland. Located near the Baltic Sea and the German border, it is a major seaport and Poland's seventh-largest city. As of December 2021, the population was 395,513. Szczecin is located on the river Oder, south of the Szczecin Lagoon and the Bay of Pomerania. The city is situated along the southwestern shore of DÄ…bie Lake, on both sides of the Oder and on several large islands between the western and eastern branches of the river. Szczecin is adjacent to the town of Police and is the urban centre of the Szczecin agglomeration, an extended metropolitan area that includes communities in the German states of Brandenburg and Mecklenburg-Western Pomerania. Szczecin is the administrative and industrial centre of West Pomeranian Voivodeship and is the site of the University of Szczecin, Pomeranian Medical Universi ...
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Parts Per Thousand
In science and engineering, the parts-per notation is a set of pseudo-units to describe small values of miscellaneous dimensionless quantities, e.g. mole fraction or mass fraction. Since these fractions are quantity-per-quantity measures, they are pure numbers with no associated units of measurement. Commonly used are parts-per-million (ppm, ), parts-per-billion (ppb, ), parts-per-trillion (ppt, ) and parts-per-quadrillion (ppq, ). This notation is not part of the International System of Units (SI) system and its meaning is ambiguous. Overview Parts-per notation is often used describing dilute solutions in chemistry, for instance, the relative abundance of dissolved minerals or pollutants in water. The quantity "1 ppm" can be used for a mass fraction if a water-borne pollutant is present at one-millionth of a gram per gram of sample solution. When working with aqueous solutions, it is common to assume that the density of water is 1.00 g/mL. Therefore, it is common to equate ...
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Salinity
Salinity () is the saltiness or amount of salt dissolved in a body of water, called saline water (see also soil salinity). It is usually measured in g/L or g/kg (grams of salt per liter/kilogram of water; the latter is dimensionless and equal to ‰). Salinity is an important factor in determining many aspects of the chemistry of natural waters and of biological processes within it, and is a thermodynamic state variable that, along with temperature and pressure, governs physical characteristics like the density and heat capacity of the water. A contour line of constant salinity is called an ''isohaline'', or sometimes ''isohale''. Definitions Salinity in rivers, lakes, and the ocean is conceptually simple, but technically challenging to define and measure precisely. Conceptually the salinity is the quantity of dissolved salt content of the water. Salts are compounds like sodium chloride, magnesium sulfate, potassium nitrate, and sodium bicarbonate which dissolve into ions ...
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Eutrophic
Eutrophication is the process by which an entire body of water, or parts of it, becomes progressively enriched with minerals and nutrients, particularly nitrogen and phosphorus. It has also been defined as "nutrient-induced increase in phytoplankton productivity". Water bodies with very low nutrient levels are termed oligotrophic and those with moderate nutrient levels are termed mesotrophic. Advanced eutrophication may also be referred to as dystrophic and hypertrophic conditions. Eutrophication can affect freshwater or salt water systems. In freshwater ecosystems it is almost always caused by excess phosphorus. In coastal waters on the other hand, the main contributing nutrient is more likely to be nitrogen, or nitrogen and phosphorus together. This depends on the location and other factors. When occurring naturally, eutrophication is a very slow process in which nutrients, especially phosphorus compounds and organic matter, accumulate in water bodies. These nutrients derive f ...
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Eutrophic
Eutrophication is the process by which an entire body of water, or parts of it, becomes progressively enriched with minerals and nutrients, particularly nitrogen and phosphorus. It has also been defined as "nutrient-induced increase in phytoplankton productivity". Water bodies with very low nutrient levels are termed oligotrophic and those with moderate nutrient levels are termed mesotrophic. Advanced eutrophication may also be referred to as dystrophic and hypertrophic conditions. Eutrophication can affect freshwater or salt water systems. In freshwater ecosystems it is almost always caused by excess phosphorus. In coastal waters on the other hand, the main contributing nutrient is more likely to be nitrogen, or nitrogen and phosphorus together. This depends on the location and other factors. When occurring naturally, eutrophication is a very slow process in which nutrients, especially phosphorus compounds and organic matter, accumulate in water bodies. These nutrients derive f ...
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Nutrients
A nutrient is a substance used by an organism to survive, grow, and reproduce. The requirement for dietary nutrient intake applies to animals, plants, fungi, and protists. Nutrients can be incorporated into cells for metabolic purposes or excreted by cells to create non-cellular structures, such as hair, scales, feathers, or exoskeletons. Some nutrients can be metabolically converted to smaller molecules in the process of releasing energy, such as for carbohydrates, lipids, proteins, and fermentation products (ethanol or vinegar), leading to end-products of water and carbon dioxide. All organisms require water. Essential nutrients for animals are the energy sources, some of the amino acids that are combined to create proteins, a subset of fatty acids, vitamins and certain minerals. Plants require more diverse minerals absorbed through roots, plus carbon dioxide and oxygen absorbed through leaves. Fungi live on dead or living organic matter and meet nutrient needs from their host. ...
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Dziwna
The Dziwna () is a channel of the Oder River in northwestern Poland, one of three straits connecting the Oder Lagoon with the Bay of Pomerania of the Baltic Sea. It separates the island of Wolin from the rest of the Polish mainland. The other two channels are the Świna and the Peene. About in length, the Dziwna forms on the eastern end of the Szczecin Lagoon, near the town of Zagórze, Kamień County. Flowing north, it passes the town of Wolin and then widens and forms a number of connected features. Towards the west the main channel of the Dziwna forms the large Kamieński Lagoon (''Polish: Zalew Kamieński''). To the east a side channel develops into the Zatoka Cicha (''Quiet Bay'', known as ''Die Maad'' before 1949), flows north through the strait of Promna as it approaches the city of Kamień Pomorski, then rejoins the Kamieński Lagoon. Between these two channels stands the small, largely agricultural island of Chrząszczewo connected to Kamień Pomorski by a single ...
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Åšwina
The Åšwina (; Pomeranian: ''Swina'') is a river in northwest Poland, between 2 and 4 km from the German border. It flows from Szczecin Lagoon to the Baltic Sea between the islands of Uznam and Wolin. It is a part of the Oder estuary, and carries about 75% of that river's waterflow (of the remainder, Peenestrom carries 15% and Dziwna 10%). It has a length of about 16 km. ÅšwinoujÅ›cie is a major town on the river. The German Empire dammed and deepened the river from 1874-1880 to create the ''Kaiserfahrt'' ( Piast canal).http://swinemuende.name/Kaseburg%20%28Karsibor,%20district%20of%20Swinemuende%29.htm. Kaseburg (Karsibor district of Swinemuende). Accessed 28-04-2012. It connects the northern part of the Åšwina directly with the Szczecin Lagoon and the Pomeranian harbor of Szczecin (Stettin). The river thus gained importance as a direct waterway to the industrial city. The territory along the river's path was transferred from Germany to Poland following World War II. ...
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Peenestrom
The Peenestrom is a river A river is a natural flowing watercourse, usually freshwater, flowing towards an ocean, sea, lake or another river. In some cases, a river flows into the ground and becomes dry at the end of its course without reaching another body of wate ...
in Mecklenburg-Vorpommern, Germany. It is 20 kilometres long and is the westernmost connection of the Szczecin Lagoon (together with the Åšwina and the Dziwna) with the Baltic Sea. It is therefore also one of the three distributary, distributaries of the Oder River, Oder. {{Coord, 54, 4, 11, N, 13, 47, 37, E, source:nlwiki_region:DE_type:waterbody, display=title Peenestrom, Rivers of Mecklenburg-Western Pomerania Straits of the Baltic Sea Straits of Germany Rivers of Germany ...
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Bay Of Pomerania
The Bay of Pomerania ( pl, Zatoka Pomorska; german: Pommersche Bucht; csb, Pòmòrskô Hôwinga) is a basin in the southwestern Baltic Sea, off the Pomeranian shores of Poland and Germany. It stretches between the northernmost tip of the island of Rugia called ''Gellort'' northwest of Cape Arkona in the west, and the village of Jarosławiec in the east. In the south, it is bounded by the islands of Usedom/Uznam and Wolin, which separate it from the Szczecin Lagoon which is flown through by the Oder River, and is connected to the bay by three straits, the Dziwna, Świna, and Peenestrom. The Bay of Greifswald with the islands of Koos and Vilm is a large sub-bay in the southwest of the Bay of Pomerania. Apart from Rugia, Usedom/Uznam, and Wolin, the islands Greifswalder Oie and Ruden also lie in the Bay of Pomerania. Maximum depth is 20 metres and salinity is about 8%. The main ports on the Bay of Pomerania are Mukran Port in Sassnitz-Mukran, the port of Świnoujście, the po ...
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