Spio martinensis Mesnil, 1896 (polychaeta, Spionidae): Not a new record in German coastal waters of the North Sea

2003 ◽  
Vol 32 (1-2) ◽  
pp. 25-33 ◽  
Author(s):  
Cord Bergfeld ◽  
Ingrid Kröncke
Keyword(s):  
North Sea ◽  
Coastal Waters ◽  
New Record ◽  
The North ◽  
The North Sea ◽  
Spio Martinensis

Temperature, Salinity and Plankton in the Eastern North Atlantic and Coastal Waters of Britain, 1957.: I. The Characterisation and Distribution of Surface Waters

1963 ◽  
Vol 20 (3) ◽  
pp. 789-826 ◽  
Author(s):  
B. McK. Bary
Keyword(s):  
North Sea ◽  
North Atlantic ◽  
Coastal Waters ◽  
Water Bodies ◽  
English Channel ◽  
Oceanic Water ◽  
Climatic Fluctuations ◽  
The North ◽  
The North Sea ◽  
Eastern North Atlantic

Monthly temperature-salinity diagrams for 1957 have demonstrated that three surface oceanic "water bodies" were consistently present in the eastern North Atlantic; two are regarded as modified North Atlantic Central water which give rise to the third by mixing. As well in the oceanic areas, large and small, high or low salinity patches of water were common. Effects of seasonal climatic fluctuations differed in the several oceanic water bodies. In coastal waters, differences in properties and in seasonal and annual cycles of the properties distinguish the waters from the North Sea, English Channel and the western entrance to the Channel.The geographic distributions of the oceanic waters are consistent with "northern" and "southern" water bodies mixing to form a "transitional" water. Within this distribution there are short-term changes in boundaries and long-term (seasonal) changes in size of the water bodies.Water in the western approaches to the English Channel appeared to be influenced chiefly by the mixed, oceanic transitional water; oceanic influences in the North Sea appear to have been from northern and transitional waters.

Mapping of the North Sea turbid coastal waters using SeaWiFS data

2004 ◽  
Vol 30 (1) ◽  
pp. 44-53 ◽  
Author(s):  
Hans van der Woerd ◽  
Reinold Pasterkamp
Keyword(s):  
North Sea ◽  
Coastal Waters ◽  
The North ◽  
The North Sea

XIV.—New Records of Polychætes from Scottish Coastal and Offshore Waters

1960 ◽  
Vol 67 (4) ◽  
pp. 351-362 ◽  
Author(s):  
A. D. McIntyre
Keyword(s):  
North Sea ◽  
Deep Water ◽  
West Coast ◽  
Coastal Waters ◽  
East Coast ◽  
New Records ◽  
North West ◽  
The North ◽  
The North Sea

SynopsisFrom a faunistic survey in Scottish waters, concentrated mainly in the sea lochs of the north-west coast and in the deep water in the North Sea off the east coast, thirty-two species of polychætes are listed which have not previously been recorded from these areas. Seven of the species are new records for British coastal waters or for the North Sea.

scholarly journals Carbon dynamics and CO<sub>2</sub> air-sea exchanges in the eutrophied coastal waters of the Southern Bight of the North Sea: a modelling study

2004 ◽  
Vol 1 (2) ◽  
pp. 147-157 ◽  
Author(s):  
N. Gypens ◽  
C. Lancelot ◽  
A. V. Borges
Keyword(s):  
Surface Water ◽  
Coastal Zone ◽  
North Sea ◽  
Coastal Waters ◽  
Co2 Flux ◽  
Open Ocean ◽  
Atmospheric Co2 ◽  
Southern Bight ◽  
The North ◽  
The North Sea

Abstract. A description of the carbonate system has been incorporated in the MIRO biogeochemical model to investigate the contribution of diatom and Phaeocystis blooms to the seasonal dynamics of air-sea CO2 exchanges in the Eastern Channel and Southern Bight of the North Sea, with focus on the eutrophied Belgian coastal waters. For this application, the model was implemented in a simplified three-box representation of the hydrodynamics with the open ocean boundary box ‘Western English Channel’ (WCH) and the ‘French Coastal Zone’ (FCZ) and ‘Belgian Coastal Zone’ (BCZ) boxes receiving carbon and nutrients from the rivers Seine and Scheldt, respectively. Results were obtained by running the model for the 1996–1999 period. The simulated partial pressures of CO2 (pCO2) were successfully compared with data recorded over the same period in the central BCZ at station 330 (51°26.05′ N; 002°48.50′ E). Budget calculations based on model simulations of carbon flow rates indicated for BCZ a low annual sink of atmospheric CO2 (−0.17 mol C m-2 y-1). On the opposite, surface water pCO2 in WCH was estimated to be at annual equilibrium with respect to atmospheric CO2. The relative contribution of biological, chemical and physical processes to the modelled seasonal variability of pCO2 in BCZ was further explored by running model scenarios with separate closures of biological activities and/or river inputs of carbon. The suppression of biological processes reversed direction of the CO2 flux in BCZ that became, on an annual scale, a significant source for atmospheric CO2 (+0.53 mol C m-2 y-1). Overall biological activity had a stronger influence on the modelled seasonal cycle of pCO2 than temperature. Especially Phaeocystis colonies which growth in spring were associated with an important sink of atmospheric CO2 that counteracted the temperature-driven increase of pCO2 at this period of the year. However, river inputs of organic and inorganic carbon were shown to increase the surface water pCO2 and hence the emission of CO2 to the atmosphere. Same calculations conducted in WCH, showed that temperature was the main factor controlling the seasonal pCO2 cycle in these open ocean waters. The effect of interannual variations of fresh water discharge (and related nutrient and carbon inputs), temperature and wind speed was further explored by running scenarios with forcing typical of two contrasted years (1996 and 1999). Based on these simulations, the model predicts significant variations in the intensity and direction of the annual air-sea CO2 flux.

The Contribution of River Systems to the Input of Pollutants to the Marine Environment in Northern Europe

1984 ◽  
Vol 16 (5-7) ◽  
pp. 83-94 ◽  
Author(s):  
R F Critchley
Keyword(s):  
North Sea ◽  
Coastal Waters ◽  
Substantial Contribution ◽  
Northern Europe ◽  
The Baltic Sea ◽  
Pollutant Load ◽  
The North ◽  
The North Sea ◽  
Main Input ◽  
The Baltic

Published information on the input of pollutants to the North Sea has been used to identify the major pollutant pathways. Rivers and atmospheric deposition are the main input routes for metals, with the Rhine/Meuse and the Elbe contributing over half the riverine input. The dumping of estuarine dredging spoils results in a very large input of metals, which cannot be fully accounted for as a redistribution of riverine material unless the river inputs have been grossly underestimated. Rivers provide the largest input route for nutrients, but a substantial contribution is also made by direct discharges to coastal waters and estuaries. Sewage sludge dumping contributes less than 5% to the pollutant load to the North Sea. Similar assessments have also been made for the Baltic Sea and the major UK estuaries.

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