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

Pub Date : 2016-12-01 DOI:10.1515/bgeo-2016-0012
B. Pius, W. Marszelewski
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引用次数: 3

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°C per 10 years, and its even faster increase in the winter season (December-March), by 0.37°C per 10 years on average. An increase in mean annual water temperature in the lake by 0.24°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.
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气候变化对热冰状态发展的影响——以波兰恰日科夫斯基湖为例
本文讨论了中欧低地Chojnice地区1961—2014年的气温变化过程及其对恰日科夫斯基湖水温和冰盖发生的影响。年平均气温每10年增加0.31°C,冬季(12月- 3月)增加更快,平均每10年增加0.37°C。湖泊年平均水温每10年增加0.24°C。冬季气温和水温的升高导致冰盖出现的时间缩短。1961—2014年,冰盖持续时间平均每10年减少3.7 d,平均冰盖厚度从30 cm减少到19 cm。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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