对芬兰北方湖泊冰融化和破裂的实地研究,Pääjärvi

IF 4.4 2区 地球科学 Q1 GEOGRAPHY, PHYSICAL Cryosphere Pub Date : 2023-05-12 DOI:10.5194/tc-17-2045-2023
Yaodan Zhang, M. Fregona, John Loehr, Joonatan Ala-Könni, Shuang Song, M. Leppäranta, Zhijun Li
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引用次数: 1

摘要

摘要湖冰融化和破裂形成了一个快速、非线性的过程,具有重要的机械、化学和生物后果。由于安全问题,该过程很难在现场进行研究,因此对其细节知之甚少。在本工作中,通过徒步、水力直升机和船收集了融化期冰厚度、结构和地球化学演变的全时间序列的现场数据。这些观测是2018年(试点研究)和2022年在Pääjärvi湖进行的。2022年,最大冰层厚度为55 厘米,带60 % 冰雪,在40 d冰融化了33 距地表22厘米 距底部厘米,而孔隙率从小于5 %至40 %–50 % 分手时。2018年,冰雪层较薄,底部和内部融化主导了冰的腐烂。平均熔化速率为1.31 厘米 2022年d−1和1.55 厘米 2018年d−1。2022年,冰的电导率(EC)为11.4 ± 5.79 µS cm−1,比湖水低1个数量级,冰的pH值为6.44 ± 0.28,比在水中低0.4。冰和水的pH值和EC在冰衰变过程中降低,但由于湖水的冲刷,冰略有增加。叶绿素a小于0.5 µg L−1在多孔冰中,大约是湖水中的三分之一。这些结果对于理解冰的衰变过程及其对湖泊生态学的影响、进一步发展湖泊冰的数值模型以及建立冰盖和冰荷载的安全模型具有重要意义。
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A field study on ice melting and breakup in a boreal lake, Pääjärvi, in Finland
Abstract. Lake ice melting and breakup form a fast, nonlinear process with important mechanical, chemical, and biological consequences. The process is difficult to study in the field due to safety issues, and therefore only little is known about its details. In the present work, the field data were collected on foot, by hydrocopter, and by boat for a full time series of the evolution of ice thickness, structure, and geochemistry through the melting period. The observations were made in lake Pääjärvi in 2018 (pilot study) and 2022. In 2022, the maximum thickness of ice was 55 cm with 60 % snow ice, and in 40 d the ice melted by 33 cm from the surface and 22 cm from the bottom while the porosity increased from less than 5 % to 40 %–50 % at breakup. In 2018, the snow-ice layer was thin, and bottom and internal melting dominated the ice decay. The mean melting rates were 1.31 cm d−1 in 2022 and 1.55 cm d−1 in 2018. In 2022 the electrical conductivity (EC) of ice was 11.4 ± 5.79 µS cm−1, which is 1 order of magnitude lower than in the lake water, and ice pH was 6.44 ± 0.28, which is lower by 0.4 than in water. The pH and EC of ice and water decreased during the ice decay except for slight increases in ice due to flushing by lake water. Chlorophyll a was less than 0.5 µg L−1 in porous ice, approximately one-third of that in the lake water. The results are important for understanding the process of ice decay with consequences for lake ecology, further development of numerical lake ice models, and modeling the safety of ice cover and ice loads.
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来源期刊
Cryosphere
Cryosphere GEOGRAPHY, PHYSICAL-GEOSCIENCES, MULTIDISCIPLINARY
CiteScore
8.70
自引率
17.30%
发文量
240
审稿时长
4-8 weeks
期刊介绍: The Cryosphere (TC) is a not-for-profit international scientific journal dedicated to the publication and discussion of research articles, short communications, and review papers on all aspects of frozen water and ground on Earth and on other planetary bodies. The main subject areas are the following: ice sheets and glaciers; planetary ice bodies; permafrost and seasonally frozen ground; seasonal snow cover; sea ice; river and lake ice; remote sensing, numerical modelling, in situ and laboratory studies of the above and including studies of the interaction of the cryosphere with the rest of the climate system.
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