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Evidence for a warm water inflow into the Baltic Proper in summer 2003

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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The exceptional warm water inflow into the Baltic Sea in summer 2002, which preceded the major Baltic inflow of January 2003, was surprisingly repeated in modified form in summer 2003. Its warm waters even replaced the renewed, cold inflow waters in the eastern Gotland Basin and commenced another warm period in its deep layers, where the previous one had lasted from 1997 to 2003. Details of the temporal and spatial behaviour of this new baroclinic inflow are presented from various measurements carried out from the Kiel Bight up to Gotland, covering the Darss Sill, the Arkona, Bornholm, Gdańsk Basins and the Słupsk Channel, focused mainly on the time period between July 2003 and July 2004. Hypothetically, the repetition of these exceptional warm inflow events could be regarded as a possible regional indicator for global climatic change.
Słowa kluczowe
Czasopismo
Rocznik
Strony
581--598
Opis fizyczny
Bibliogr. 20 poz., mapa, tab., wykr..
Twórcy
autor
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
  • Institute of Oceanology, Polish Academy of Sciences, Powstańców Warszawy 55, PL-81-712 Sopot, Poland
autor
  • Baltic Sea Research Institute, Seestrasse 15, D-18119 Rostock-Warnemünde, Germany
Bibliografia
  • [1] Chuine I., Yiou P., Viovy N., Seguin B., Daux V., Le Roy Ladurie E., 2004, Historical phenology: grape ripening as a past climate indicator, Nature, 432, 89-290.
  • [2] DWD (Deutscher Wetterdienst), 2003, Witterungsreport Daten, Jg. 5 (Jahresausgabe 2003), 23 pp.
  • [3] Feistel R., 1999, New shoreline map-drawing data available, Eos Trans. Am. Geophys. Union, 80 (22), 249 pp., Electron. Suppl., [http://earth.agu.org/eos_elec/99063e.html].
  • [4] Feistel R., 2004, IOW Cruise Report 11/04/03, March 2004, [http://www.io-warnemuende.de/projects/monitoring/documents/cr110403.pdf].
  • [5] Feistel R., Nausch G., Matthäus W., Hagen E., 2003a, Temporal and spatial evolution of the Baltic deep water renewal in spring 2003, Oceanologia, 45 (4), 623-642, [http://www.iopan.gda.pl/oceanologia/454feis2.pdf].
  • [6] Feistel R., Nausch G., Matthäus W., Łysiak-Pastuszak E., Seifert T., Sehested Hansen I., Mohrholz V., Krüger S., Buch E., Hagen E., 2004, Background data to the exceptionally warm inflow into the Baltic Sea in late summer of 2002, Meereswiss. Ber. (Warnemünde), 58, 1-58, [http://www.io-warnemuende.de/research/mebe.html].
  • [7] Feistel R., Nausch G., Mohrholz V., Łysiak-Pastuszak E., Seifert T., Matthäus W., Krüger S., Sehested Hansen I., 2003b, Warm waters of summer 2002 in the deep Baltic Proper, Oceanologia, 45 (4), 571-592, [http://www.iopan.gda.pl/oceanologia/454feis1.pdf].
  • [8] Hagen E., Feistel R., 2001, Spreading of Baltic deep water: a case study for the winter 1997-1998, Meereswiss. Ber. (Warnemünde), 45, 99-133, [http://www.io-warnemuende.de/research/mebe.html].
  • [9] Hagen E., Feistel R., 2004, Observations of low-frequency current fluctuations in deep water of the Eastern Gotland Basin/Baltic Sea, J. Geophys. Res., 109 (C03044), 1-15, [doi: 10.1029/2003JC002017].
  • [10] 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/combine-home.htm].
  • [11] Jost G., 2003, IOW Cruise Report 44/03/08, August 2003, [http://www.io-warnemuende.de/edv-intern/dienst/exberichte/f_cr03029.doc].
  • [12] Karstensen J., 2003, BASEWECS Cruise Report AL229, IfM Kiel, September 2003, [http://www.ifm.uni-kiel.de/fb/fb1/po2/edu/praktikum/ss03_hf/ss03_hf.html].
  • [13] Kraus G., Möllmann C., Hinrichsen H.-H., Lehmann A., Schnack D., 2003, Unusual water mass advection affected Central Baltic key species 1: Sprat and the summer inflow, GLOBEC Int. Newslett., 9 (2), 27-28, [http://www.pml.ac.uk/globec/Publications/Newsletter/Newsletter.htm].
  • [14] Kuβ J., 2003, IOW Cruise Report 44/03/09, August 2003, [http://www.io-warnemuende.de/edv-intern/dienst/exberichte/f03030.doc].
  • [15] Matthäus W., Francke E., Lass H. U., Schwabe R., 1982, Untersuchungen der Wasseraustauschprozesse im Bereich der Darsser Schwelle, Beitr. Meereskunde., 47, 31-50.
  • [16] Nausch G., Feistel R., Lass H.-U., Nagel K., Siegel H., 2004, Hydrographisch-chemische Zustandseinschätzung der Ostsee 2003, Meereswiss. Ber. (Warnemünde), 59, 1-80, [http://www.io-warnemuende.de/research/mebe.html].
  • [17] Piechura J., Beszczyńska-Möller A., 2004, Inflow waters in the deep regions of the southern Baltic Sea – transport and transformations, Oceanologia, 46 (1), 113-141, [http://www.iopan.gda.pl/oceanologia/46_1.html].
  • [18] Seifert T., Tauber F., Kayser B., 2001, A high resolution spherical grid topography of the Baltic Sea – 2nd edition, Baltic Sea Sci. Congr., Stockholm 25-29 November 2001, Poster #147, [http://www.io-warnemuende.de/research/de_iowtopo.html].
  • [19] Stott, P. A., Stone, D. A., Allen, M. R., 2004, Human contribution to the European heatwave of 2003, Nature, 432, 610-614.
  • [20] Wasmund N., 2003, IOW Cruise Report 44/03/07, August 2003, [http://www.io-warnemuende.de/projects/monitoring/documents/cr440307.pdf].
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BUS5-0011-0080
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