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Effect of climatic changes on the development of the thermal-ice regime based on the example of Lake Charzykowskie (Poland)

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dc.contributor.author Pius, Bożena
dc.date.accessioned 2017-04-19T09:19:30Z
dc.date.available 2017-04-19T09:19:30Z
dc.date.issued 2017-01-09
dc.identifier.citation Bulletin of Geography. Physical Geography Series, No. 11, pp. 27-33
dc.identifier.issn 2300-8490
dc.identifier.other doi:10.2478/11170
dc.identifier.uri http://repozytorium.umk.pl/handle/item/4174
dc.description.abstract Abstract. The paper discusses the course of air temperature in the years 1961-2014 in Chojnice (Central European Lowland), and its effect on water temperature and occurrence of ice cover on Lake Charzykowskie. An increase in mean annual air temperature was determined by 0.31 o C per 10 years, and its even faster increase in the winter season (December-March), by 0.37 o C per 10 years on average. An increase in mean annual water temperature in the lake by 0.24 o C per 10 years also occurred. An increase in air and water temperature in winter months caused a reduction of the period of occurrence of ice cover. In the years 1961-2014, the persistence of ice cover was subject to a decrease by 3.7 days per 10 years on average, and the mean thickness of  the ice cover decreased from 30 to 19 cm.
dc.language.iso eng
dc.rights Attribution-NoDerivs 3.0 Poland
dc.rights info:eu-repo/semantics/openAccess
dc.rights.uri http://creativecommons.org/licenses/by-nd/3.0/pl/
dc.title Effect of climatic changes on the development of the thermal-ice regime based on the example of Lake Charzykowskie (Poland)
dc.type info:eu-repo/semantics/article


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