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Tytuł artykułu

Hydrographic and hydrochemical conditions in the Gotland Deep area between 1992 and 2003

Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The paper describes the hydrographic-hydrochemical development in the eastern Gotland Basin between the major saltwater inflows into the Baltic Sea in 1993 and 2003. This period is characterised by only low inflow activity. The most important hydrographic events were the effects of the very strong inflow in 1993 and the weak inflows in 1993/1994 and 1997. The 1993/1994 inflows led to deep-water renewal, a steep fall in deep-water temperatures, and increasing salinity. The effects of the inflow of very warm, saline and oxygen-rich water in autumn 1997 were observed in the deep water in 1998, resulting in temperatures rising to 7°C. The recent renewal in spring 2003 is reflected in the decreasing temperature, higher salinity and improved ventilation of the bottom water. Changes in the redox conditions exert a considerable influence on the nutrient distribution. During stagnation periods, there is enrichment of phosphate and ammonium, while nitrate is absent. Thus, around 31 žmol l-1 ammonium and 7 žmol l-1 phosphate were measured prior to the water renewal in 2003. Deep-water ventilation results in lower phosphate concentrations of around 2 žmol l-1, the nitrification of ammonium and the occurrence of nitrate. For the observation period, an estimate of nutrients stored in the deep water was done for the eastern Gotland Basin. During the recent stagnation period, there was an increase of up to 150% in the phosphate pool below the halocline, whereas the pool of inorganic nitrogen compounds decreased to 80% compared with 1992 when the previous stagnation period had ended. Under specific circumstances, these unbalanced nutrients can be made available to the upper water layers and can induce large-scale blooms of algae, especially of cyanobacteria.
Czasopismo
Rocznik
Strony
557--569
Opis fizyczny
Bibliogr. 25 poz., tab., wykr.
Twórcy
autor
  • Baltic Sea Research Institute, Seestrasse 15, D-18119 Rostock-Warnemünde, Germany
autor
  • Baltic Sea Research Institute, Seestrasse 15, D-18119 Rostock-Warnemünde, Germany
autor
  • Baltic Sea Research Institute, Seestrasse 15, D-18119 Rostock-Warnemünde, Germany
Bibliografia
  • [1] Feistel R., Nausch G., Hagen E., 2003a, The Baltic inflow of autumn 2001, Meereswiss. Ber., 54, 55-68, http://www.io-warnemuende.de/research/mebe.html.
  • [2] Feistel R., Nausch G., Matthäus W., Hagen E., 2003b, Temporal and spatial evolution of the Baltic deep water renewal in spring 2003, Oceanologia, 45 (4), 623-642.
  • [3] Grasshoff K., Ehrhardt M., Kremling K., 1983, Methods of seawater analysis, (2nd edn.) Verl. Chem., Weinheim, 419 pp.
  • [4] Hagen E., Feistel R., 2001, Spreading of Baltic deep water: a case study for the winter 1997-1998, Meereswiss. Ber., 45, 99-133, http://www.io-warnemuende.de/research/mebe.html.
  • [5] Håkansson B., Broman B., Dahlin H., 1993, The flow of water and salt in the Sound during the Baltic major inflow event in January 1993, Proc. ICES Statutory Meeting, Dublin, ICES-C.M. C:57, 26 pp.
  • [6] HELCOM, 2002, Manual of marine monitoring in the COMBINE programme of HELCOM, Baltic Mar. Environ. Prot. Commiss., Helsinki, (updated 2001/2002), http://www.helcom.fi/mons/combinemanual2/combinehome.html.
  • [7] Jakobsen F., 1995, The major inflow to the Baltic Sea during January 1993, J. Mar. Sys., 6, 227-240.
  • [8] Matthäus W., 1990, Langzeittrends und Veränderungen ozeanologischer Parameter während der gegenwärtigen Stagnationsperiode im Tiefenwasser der zentralen Ostsee, Fischerei-Forsch. Rostock, 28 (3), 25-34.
  • [9] Matthäus W., Franck H., 1992, Characteristics of major Baltic inflows – a statistical analysis, Cont. Shelf Res., 12, 1375-1400.
  • [10] Matthäus W., Lass H. U., 1995, The recent salt inflow into the Baltic Sea, J. Phys. Oceanogr., 25, 280-286.
  • [11] Matthäus W., Nausch G., 2003, Hydrographic-hydrochemical variability in the Baltic Sea during the 1990s in relation to changes during the 20th century, ICES Mar. Sci. Symp., 219, 132-143.
  • [12] Matthäus W., Nausch G., Lass H. U., Nagel K., Siegel H., 1998, The Baltic Sea in 1997 – impacts of the extremely warm summer and of the exceptional Oder flood, Dt. Hydrogr. Z., 50 (1), 47-69.
  • [13] Matthäus W., Nausch G., Lass H. U., Nagel K., Siegel H., 1999, The Baltic Sea in 1998 – characteristic features of the current stagnation period, nutrient conditions in the surface layer and exceptionally high deep water temperatures, Dt. Hydrogr. Z., 51 (1), 67-84.
  • [14] Matthäus W., Nausch G., Lass H. U., Nagel K., Siegel H., 2001, The Baltic Sea in 1999 – stabilization of nutrient concentrations in the surface water and increasing extent of oxygen deficiency in the central Baltic deep water, Meereswiss. Ber., 45, 3-25.
  • [15] Matthäus W., Nehring D., Lass H. U., Nausch G., Nagel K., Siegel H., 1997, Hydrographisch-chemische Zustandseinschätzung der Ostsee 1996, Meereswiss. Ber., 24, 1-49.
  • [16] Nausch G., Feistel R., Lass H. U., Nagel K., Siegel H., 2002, Hydrographisch-chemische Zustandseinschätzung der Ostsee 2001, Meereswiss. Ber., 49, 2-77.
  • [17] Nausch G., Feistel R., Lass H. U., Nagel K., Siegel H., 2003, Hydrographisch-chemische Zustandseinschätzung der Ostsee 2002, Meereswiss. Ber., 55, 1-71.
  • [18] Nausch G., Nehring D., 1994, Nutrient dynamics in the Gotland Deep – reactions to the major salt water inflow in 1993, Vol. 2, pp. 551-559, Proc. 19th Conf. Baltic Oceanogr., 29 August-1 September 1994, Sopot.
  • [19] Nehring D., Matthäus W., 1991, Current trends in hydrographic and chemical parameters and eutrophication in the Baltic Sea, Int. Rev. ges. Hydrobiol., 76, 297-316.
  • [20] Nehring D., Matthäus W., Lass H. U., 1993, Die hydrographisch-chemischen Bedingungen in der westlichen und zentralen Ostsee im Jahre 1992, Dt. Hydrogr. Z., 45, 281-312.
  • [21] Nehring D., Matthäus W., Lass H. U., Nausch G., 1994, Die hydrographisch-chemischen Bedingungen in der westlichen und zentralen Ostsee im Jahre 1993, Dt. Hydrogr. Z., 46, 151-162.
  • [22] Nehring D., Matthäus W., Lass H. U., Nausch G., Nagel K., 1995a, The Baltic Sea 1994 – consequences of the hot summer and inflow events, Dt. Hydrogr. Z., 47, 131-144.
  • [23] Nehring D., Matthäus W., Lass H. U., Nausch G., Nagel K., 1995b, The Baltic Sea 1995 – beginning of a new stagnation period in its central Baltic deep waters and decreasing nutrient load in its surface waters, Dt. Hydrogr. Z., 47, 319-327.
  • [24] Schneider B., Nausch G., Kubsch H., Petersohn I., 2002, Accumulation of total CO2 during stagnation in the Baltic deep water and its relationship to nutrient and oxygen concentrations, Mar. Chem., 77, 277-291.
  • [25] Seifert T., Kayser B., 1995, A high resolution spherical grid topography of the Baltic Sea, Meereswiss. Ber., 9, 72-88.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BUS8-0013-0081
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