Yaodan Zhang, M. Fregona, John Loehr, Joonatan Ala-Könni, Shuang Song, M. Leppäranta, Zhijun Li
{"title":"对芬兰北方湖泊冰融化和破裂的实地研究,Pääjärvi","authors":"Yaodan Zhang, M. Fregona, John Loehr, Joonatan Ala-Könni, Shuang Song, M. Leppäranta, Zhijun Li","doi":"10.5194/tc-17-2045-2023","DOIUrl":null,"url":null,"abstract":"Abstract. Lake ice melting and breakup form a fast, nonlinear process with\nimportant mechanical, chemical, and biological consequences. The process is\ndifficult to study in the field due to safety issues, and therefore only\nlittle is known about its details. In the present work, the field data were\ncollected on foot, by hydrocopter, and by boat for a full time series of the\nevolution of ice thickness, structure, and geochemistry through the melting\nperiod. The observations were made in lake Pääjärvi in 2018\n(pilot study) and 2022. In 2022, the maximum thickness of ice was 55 cm with\n60 % snow ice, and in 40 d the ice melted by 33 cm from the surface\nand 22 cm from the bottom while the porosity increased from less than 5 %\nto 40 %–50 % at breakup. In 2018, the snow-ice layer was thin, and bottom\nand internal melting dominated the ice decay. The mean melting rates were\n1.31 cm d−1 in 2022 and 1.55 cm d−1 in 2018. In 2022 the\nelectrical conductivity (EC) of ice was 11.4 ± 5.79 µS cm−1, which is\n1 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\ndecreased during the ice decay except for slight increases in ice due to\nflushing by lake water. Chlorophyll a was less than 0.5 µg L−1 in\nporous ice, approximately one-third of that in the lake water. The results\nare important for understanding the process of ice decay with consequences\nfor lake ecology, further development of numerical lake ice models, and\nmodeling the safety of ice cover and ice loads.\n","PeriodicalId":56315,"journal":{"name":"Cryosphere","volume":null,"pages":null},"PeriodicalIF":4.4000,"publicationDate":"2023-05-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":"{\"title\":\"A field study on ice melting and breakup in a boreal lake, Pääjärvi, in Finland\",\"authors\":\"Yaodan Zhang, M. Fregona, John Loehr, Joonatan Ala-Könni, Shuang Song, M. Leppäranta, Zhijun Li\",\"doi\":\"10.5194/tc-17-2045-2023\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Abstract. Lake ice melting and breakup form a fast, nonlinear process with\\nimportant mechanical, chemical, and biological consequences. The process is\\ndifficult to study in the field due to safety issues, and therefore only\\nlittle is known about its details. In the present work, the field data were\\ncollected on foot, by hydrocopter, and by boat for a full time series of the\\nevolution of ice thickness, structure, and geochemistry through the melting\\nperiod. The observations were made in lake Pääjärvi in 2018\\n(pilot study) and 2022. In 2022, the maximum thickness of ice was 55 cm with\\n60 % snow ice, and in 40 d the ice melted by 33 cm from the surface\\nand 22 cm from the bottom while the porosity increased from less than 5 %\\nto 40 %–50 % at breakup. In 2018, the snow-ice layer was thin, and bottom\\nand internal melting dominated the ice decay. The mean melting rates were\\n1.31 cm d−1 in 2022 and 1.55 cm d−1 in 2018. In 2022 the\\nelectrical conductivity (EC) of ice was 11.4 ± 5.79 µS cm−1, which is\\n1 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\\ndecreased during the ice decay except for slight increases in ice due to\\nflushing by lake water. Chlorophyll a was less than 0.5 µg L−1 in\\nporous ice, approximately one-third of that in the lake water. The results\\nare important for understanding the process of ice decay with consequences\\nfor lake ecology, further development of numerical lake ice models, and\\nmodeling the safety of ice cover and ice loads.\\n\",\"PeriodicalId\":56315,\"journal\":{\"name\":\"Cryosphere\",\"volume\":null,\"pages\":null},\"PeriodicalIF\":4.4000,\"publicationDate\":\"2023-05-12\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"1\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Cryosphere\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://doi.org/10.5194/tc-17-2045-2023\",\"RegionNum\":2,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"GEOGRAPHY, PHYSICAL\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Cryosphere","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.5194/tc-17-2045-2023","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOGRAPHY, PHYSICAL","Score":null,"Total":0}
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.
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.