Struktur und Funktion der Küstengewässer

Schlungbaum, G.; Baudler, Henning

doi:10.1007/978-3-642-57113-8_2

Cited by 4 publications

(2 citation statements)

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“…The Darss-Zingst Bodden Chain (DZBC) is one of the shallow areas of inner coastal waters, known locally as 'Bodden', on the southern coast of the Baltic Sea (Schlungbaum & Baudler 2000). It is subdivided into several basins connected by narrow streams.…”

Section: Study Sitesmentioning

confidence: 99%

Long term water level and surface temperature changes in the lagoons of the southern and eastern Baltic

et al. 2011

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The paper studies variations in the water level and surface temperature of coastal lagoons along the southern and south-eastern shores of the Baltic Sea: the Curonian Lagoon, Vistula Lagoon, and Darss-Zingst Bodden Chain. Linear regressions forThe complete text of the paper is available at http://www.iopan.gda.pl/oceanologia/ Open access under CC BY-NC-ND license.I. Dailidienė, H. Baudler, B. Chubarenko, S. Navrotskaya annual mean water level variations showed a positive trend in water level, but at different rates. The highest rate during the period between 1961-2008 was recorded for the Curonian and Vistula lagoons (∼ 4 mm year −1 ), the lowest for the Darss-Zingst Bodden Chain (approximately ∼ 1 mm year −1 ). The warming trend of the mean surface water temperature in the lagoons was 0.03 • C year −1 in the period 1961-2008. Moreover, the variability in annual water temperature and sea level as well as their extreme values have increased most dramatically since the 1980s.

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Section: Study Sitesmentioning

confidence: 99%

Long term water level and surface temperature changes in the lagoons of the southern and eastern Baltic

et al. 2011

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“…Coastal waters, particularly inner coastal waters with pronounced salt gradients, are transitional areas between limnic waters and marine systems [1]. They are characterised by a morphological diversity, but also by a significant temporal and spatial variability of abiotic and biotic parameters that are caused, amongst others, by fluctuations of water level and salinity.…”

Section: Introductionmentioning

confidence: 99%

Nutrient accumulation and nutrient retention in coastal waters – 30 years investigation in the Darss‐Zingst Bodden chain

Selig¹,

Baudler

Krech

et al. 2006

Acta hydrochim. hydrobiol.

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Coastal waters are transitional zones between limnic waters and marine systems. The anthropogenic impact on these water bodies is high and a rapid change of trophic level was observed within the last 50 years. In the Darss-Zingst Bodden chain (southern Baltic Sea -MecklenburgWest Pomerania, Germany), the change in trophic state during the last thirty years can be reconstructed by long-term monitoring of chemical, hydrographical and biological parameters with an up to daily resolution. Until the 1980s, increased input of the anthropogenic nutrient load from the catchment area has been documented. However, with the implementation of the HELCOM recommendations the input of phosphorus and nitrogen was reduced in the 1990s. In contrast to the reduction of nutrient inputs, a decrease in nutrient concentrations and primary production could not be observed. The reasons are a high internal nutrient load and the release of nutrients out of the sediments. Numerous research projects allowed the description and quantification of these processes. Today, the internal phosphorus pool exceeds the external phosphorus load several fold. These results are the scientific basis for the development of restoration strategies of coastal waters. The development of suitable management plans is necessary for the implementation of the EU Water Framework Directive to guarantee a good ecological state by 2015. The long time acquisition of monitoring data and voluminous complementary specific research projects was enabled by the local field research conditions of the Biological Station of the University of Rostock in Zingst.

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