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

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