Zlodzenie Zatoki Admiralicji w latach 1977-1996 (Wyspa Króla Jerzego, Szetlandy Południowe)

• Autorzy: Kruszewski G.

Warianty tytułu

EN

Ice conditions in the Admiralty Bay since 1977 to 1996 (King George Island, South Shetland Islands)

• Języki publikacji: PL

Abstrakty

EN

Ice conditions are one of the most difficult to analyse, because of number of factors having influence on it. The analysed historical data from the past 20 years were difficult to verify, because of the lack of the systematic observations ice conditions. The number and scale of factors, having influence on ice cover being built up and disintegrated are too large to analyse them one by one. In such case it is more easy to create “ice conditions categories, which will characterise main conditions of ice cover in different years (seasons). The presented ice categories in on easy way describe features of ice conditions intensity in the waters the Admiralty Bay waters. Using them it is easy to show the changeability phenomenon, difficult to explain in a different way, because of too large number of possible factors - different in different seasons – having influence on ice formation and disintegration. Ice conditions categories play the role of the 'local factor' in ice phenomena variations in the analysed area. Ice condition categories as shown in Table 1 are strong and significant correlated on level r = 0.705 (Spearman correlation) with values of AlGl given by Hewitt (1997), which describe ice extent during a year on the area 104 larger than the Admiralty Bay.

Słowa kluczowe

PL

zjawiska lodowe; Zatoka Admiralicji; zlodzenie

EN

ice phenomena; Admiralty Bay; ice conditions

• Wydawca: Stowarzyszenie Klimatologów Polskich
• Czasopismo: Problemy Klimatologii Polarnej
• Rocznik: 1999
• Tom: nr 9
• Strony: 173--191
• Opis fizyczny: Bibliogr. 14 poz., rys., tab.

Twórcy

autor

Kruszewski G.

• Katedra Meteorologii i Oceanografii Nautycznej, Wydział Nawigacyjny Wyższej Szkoły Morskiej w Gdyni

Bibliografia

• 1. Barański A., Grabiec J., 1989. Meteorological data from Polis Antarctic Station "H.Arctowski" for 1988. Pol. Polar Res., 10, 255-258.
• 2. Fedak K., Gerstmann K., Marsz A 1985. Zatoka Admiralicji. Opis locyjny (Admiralty Bay. Sailing directions). WSM Gdynia, ss.80.
• 3. Hewitt. R.P. 1997. Areal and seasonal extent of sea-ice cover off the Northwestern side of the Antarctic Peninsula: 1979 to 1996. CCAMLR Science, Vol. 4, 65-73
• 4. Kowalski D., Wielbińska D., 1989. Synoptic features of severe winter 1986 at Arctowski Station, King George Island, West Antarctica. Pol. Polar Res., 10, 57-71.
• 5. Kruszewski G. 1996. Przebieg zjawisk lodowych na Zatoce Admiralicji w roku 1995 i ich związek z warunkami pogodowymi. (Ice phenomena in Admiralty Bay in 1995 and their relations with weather conditions). Probl. Klimatol. Polarnej, WSM Gdynia, 6,159-178.
• 6. Lipski M 1987. Variations of physical conditions, nutrients and chlorophyll contents in Admiralty Bay (King George Island, South Shetland Islands, 1979). Pol. Polar Res, 8, 307-332.
• 7. Madejski P., Rakusa-Suszczewski S. 1990. Icebergs as tracers of water movement in Bransfield Strait. Antarctic Science 2 (3), 259-263.
• 8. Nemec J., Rawa Z, 1989. Meteorological data fram Polish Antarctic Station "H.Arctowski" for 1987. Pol. Polar Res., 10,251-254.
• 9. Presler P., 1980. Phenological and physiographical observations carried out during the first wintering at the Arctowski Station in 1977. Pol. Arch. Hydrobiol. 27, 245-252.
• 10. Pruszak Z. 1980. Currents circulation in the waters of Admiralty Bay (region of Arctowski Station on King George Island). Pol. Polar Res, 1, 55-74.
• 11. Rakusa-Suszczewski S. 1995. The hydrography of Admiralty Bay and its inlets, coves and lagoons (King George Island, Antarctica) Pol. Polar Res., 16, 61-70.
• 12. Terminologia lodów morskich WMO, 1981 IMGW, WK i Ł, Warszawa; 35 pp.
• Inne źródła danych:
• 13. Raporty i sprawozdania kierowników wypraw oraz kroniki wypraw antarktycznych. Własność ZBA PAN
• 14. Kejna M. - Sprawozdanie "Temperatura wody morskiej w strefie brzegowej oraz zjawiska lodowe Zatoki Admiralicji w okresie od 17 grudnia 1995 do 13 grudnia 1996 r." (rękopis).