气候变化期间波罗的海集水区南部和东部湖泊的热量机制

R. Skowron, Tomasz Jaszczyk
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引用次数: 0

摘要

该研究涵盖了位于波兰北部和白俄罗斯的 11 个湖泊,旨在确定 1971-2020 年地表水温度变化的程度和趋势,以及 1961-2020 年期间在持续气候变化影响下湖泊冰盖的情况。分析的重点是月平均地表水温度(SWT)的变化和趋势,以及冰盖的开始和结束、持续时间和最大厚度的变化。这些湖泊的年平均地表水温平均每年上升 0.044°C。变化趋势最大的湖泊是切尔沃诺湖(Chervonoe),每年上升 0.066°C,而变化趋势最小的是哈尔扎湖(Hańcza),每年上升 0.029°C。冰盖持续时间每年减少 0.6 天,最大冰层厚度每年减少 0.27 厘米。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Thermal regimes of lakes in the southern and eastern part of the Baltic Sea catchment area during the period of climate change
  The study covered eleven lakes located in northern Poland and Belarus, aiming to determine the degree and trends of surface water temperature changes for the years 1971–2020 and lake ice cover  for  the  period  of  1961–2020  under  the  influence  of  ongoing  climate  changes.  The  analysis focused on changes and trends in average monthly surface water temperatures (SWT), as well as changes  in  the  onset  and  end,  duration  and  maximum  thickness  of  ice  cover.  The  average  annual surface water temperature increased in the lakes by an average of 0.044°C per  year. The lake with the highest trend is Chervonoe, at with 0.066°C per year, while the lowest is 0.029°C per year in Lake Hańcza. The ice  cover duration  showed a decrease of 0.6 days per year, and there was a reduction in maximum ice thickness of 0.27 cm per year  
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