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Baltic Navigation in Ice in the Twenty First Century

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EN
Abstrakty
EN
The Baltic Sea, even though not large in the global scale, is an important shipping lane. In winter, especially in the region of the Gulf of Bothnia, navigation is seriously obstructed by ice. The aim of this work was investigation of changes in the intensity of the obstruction by ice, caused by climate change in coming 90 years of the twenty first century. It was one of the first attempts of technical application of the global climate scenarios effects. It should be stressed, that the presented work results (as application of the climate scenarios), couldn’t be treated as forecast, as it is only the changes tendency assessment. The climate changes were examined as the changes in air temperature (adaptation of global emission models to regional scale) and atmospheric pressure gradient (model ECHAM5), according to three global scenarios B, A2 and A1B. The number of cases, in which Swedish and Finnish icebreakers assisted the ships, was assumed as the indicator of navigation obstruction by ice “K”. The severity of sea ice conditions was presented by the indicator “S”, calculated as the mean value of regional indices. The “S” is the function of the number of days with sea ice, observed at the stations in the particular regions and probability of the sea ice appearances. Relations between sea ice severity index “S” and regional climate parameters (monthly and annual air temperature and atmospheric pressure gradient ) were calculated for the calibration period of 1956-2004. Three models were build: model 1a. “thermal” (the dependence on the mean monthly temperature of July and December); model 1b. thermal “B” (the function of average annual air temperature and of the mean monthly December temperature) and model 2 “thermal zonal” (the dependence on the mean temperature of July and December and zonal component of air pressure gradient). The level of approximation was similar for the analyzed models (over 0,6). Calculation of the future (in XXI century) changes of indicator “K” was done according to three scenarios B, A1B and A2. The number of icebreakers’ assistance events should be lower than the one in the twentieth century. The lowest intensity of this decrease is estimated by model 2 and scenario A1Br1, the highest one – for model M1b and scenario B r1. Otherwise, the minimum value, calculated for the scenarios, is higher than in a period of 1956-2004. It means, that probably, the period with obstruction for navigation in ice could be longer, but not as severe as in the period of 1956-2004. The obstruction intensity could increase during the 21 century according to scenario B1r1, the same for empirical model 2. The similar tendency has been shown by scenario A1Br1 and by model 1a. Other models and scenarios estimated the decreasing trend up to 2100.
Twórcy
autor
  • Institute of Meteorology and Water Management - National Research Institute, Maritime Branch, Gdynia, Poland
Bibliografia
  • [1] Jakusik E. , Marosz M., Pilarski M., Mietus M, 2010 :Wpływ pola barycznego na wysokość falowania wiatrowego w południowej części Morza Bałtyckiego. Materiały Geo-Sympozjum Młodych badaczy Silesia, 1-14,
  • [2] Jakusik E, Wójcik R., Biernacik D., Miętus M., 2010: Wpływ zmian pola barycznego nad Europą i Północnym Atlantykiem na zmiany średniego poziomu Morza Bałtyckiego w strefie polskiego wybrzeża , w Woda w badaniach geograficznych, UJK Kielce, 59-74
  • [3] Kalnay et al., 1996, The NCEP/NCAR 40-year Reanalysis Project, Bull. Amer. Meteor. Soc., 77, 437-471
  • [4] Mietus M., 1999, The role of atmospheric circulation over Europe and North Atlantic in forming climatic and oceanographic conditions in the Polish coastal zone, Materialy Badawcze IMGW, seria Meteorologia, 29, 157 pp. (in Polish),
  • [5] Mietus M., (main editor), 2009: Report of KLIMAT project, www.klimat.imgw.pl,
  • [6] Mietus M., ., (main editor) 2010 Report of KLIMAT project, www.klimat.imgw.pl,
  • [7] Schmelzer N., Seina A., Lundqvist J.E., Sztobryn M., 2008, Ice, in: State and Evolution of the Baltic Sea, 1952-2005, Wiley & Sons, 199-240,
  • [8] Storch von H., Zwiers F., 2001, Statistical analysis in climate research, Cambridge Univ. Press, 499 pp.
  • [9] Sztobryn M.,2006, Sea ice condition – Polish coastal waters 1955-2005, IMGW, Report of Project DS.-H7, (in Polish)
  • [10] Sztobryn M., Schmelzer N., Vainio J., Eriksson P.B., 2009. „Sea Ice Index”. Report Series in Geophysics, University of Helsinki, No 61, 82-91, Helsinki 2009
  • [11] Sztobryn M., R.Wójcik, 2010, Impact of climate change on the Baltic sea ice conditions, 20th IAHR International Symposium on Ice, Finland,
  • [12] Werner P. C., Storch von H., 1993, Interannual variability of Central Europe mean temperature in January-February and its relation to large-scale circulation, Climate Research 3, 195-207
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-a76c5daa-c167-4049-a189-4217d5ef2c8c
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