Drivers of spatio-temporal variations in summer surface water temperatures of Arctic Fennoscandian lakes (2000–21)

IF 1.9 4区 地球科学 Q3 ECOLOGY Polar Research Pub Date : 2024-08-08 DOI:10.33265/polar.v43.9580
Mingzhen Zhang, Matti Leppäranta, A. Korhola, Nina Kirchner, A. Granebeck, Frederik Schenk, K. Weckström, Maija Heikkilä, J. Weckström
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Abstract

The Arctic region is covered with numerous small lakes whose ecosystems are vulnerable to current climate warming and resultant changes in water temperature, ice-cover duration and lake levels. Data on thermal features of these lakes are sparse, which hinders our understanding of the possible ecosystem impacts of the warming climate and climate feedbacks at larger spatial scales. We investigated spatial–temporal variations of lake surface water temperatures (LSWT) in 12 Arctic lakes in north-west Finnish Lapland and explored the predominant drivers of LSWTs by continuous year-round observations. The lake surface temperature data were recorded using thermistors at bi-hourly resolution during the years 2000, 2007–08 and 2019–2021. A large regional heterogeneity was observed in the timing of the maximum and minimum LSWTs and the overall patterns of the annual cycle. Our results reveal that July air temperature, maximum lake depth and altitude explained most of the variance in the summer LSWT (> 85%). The remaining variance was related to geographic location (longitude and latitude), lake morphometric features, such as lake area and catchment area, and certain physico-chemical characteristics, such as Secchi depth and dissolved organic carbon content. Our results provide new insights into thermal responses of different types of small Arctic lakes to climate change.
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北极芬诺斯坎迪亚湖泊夏季地表水温度时空变化的驱动因素(2000-21)
北极地区有许多小湖泊,其生态系统很容易受到当前气候变暖以及由此导致的水温、冰覆盖时间和湖泊水位变化的影响。有关这些湖泊热特征的数据非常稀少,这阻碍了我们在更大空间尺度上了解气候变暖和气候反馈可能对生态系统造成的影响。我们研究了芬兰拉普兰西北部 12 个北极湖泊的湖泊表面水温(LSWT)的时空变化,并通过全年连续观测探索了湖泊表面水温的主要驱动因素。在 2000 年、2007-08 年和 2019-2021 年期间,使用热敏电阻以每两小时一次的分辨率记录了湖泊表面温度数据。在最高和最低 LSWTs 的时间以及年周期的整体模式方面,观察到很大的区域异质性。我们的研究结果表明,7 月气温、最大湖泊深度和海拔高度解释了夏季 LSWT 的大部分变异(> 85%)。其余变异与地理位置(经度和纬度)、湖泊形态特征(如湖泊面积和汇水面积)以及某些物理化学特征(如塞奇深度和溶解有机碳含量)有关。我们的研究结果为了解不同类型的北极小湖对气候变化的热响应提供了新的视角。
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来源期刊
Polar Research
Polar Research 地学-地球科学综合
CiteScore
3.20
自引率
5.30%
发文量
22
审稿时长
>12 weeks
期刊介绍: Since 1982, Polar Research has been the international, peer-reviewed journal of the Norwegian Polar Institute, Norway''s central institution for research, environmental monitoring and mapping of the polar regions. Aiming to promote the exchange of scientific knowledge about the Arctic and Antarctic across disciplinary boundaries, Polar Research serves an international community of researchers and managers. As an open-access journal, Polar Research makes its contents freely available to the general public. Original primary research papers comprise the mainstay of Polar Research. Review articles, brief research notes, letters to the editor and book reviews are also included. Special issues are published from time to time. The scope of Polar Research encompasses research in all scientific disciplines relevant to the polar regions. These include, but are not limited to, the subfields of biology, ecology, geology, oceanography, glaciology and atmospheric science. Submissions from the social sciences and those focusing on polar management and policy issues are welcome. Contributions about Antarctica are particularly encouraged.
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