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Fluctuations of ice in a lake due to the impact of the North Atlantic Oscillation (1960/61–2009/10) – a case study of Łebsko Lake
•For coastal lakes, a constant decrease in the number of days with ice is observed•A decrease in the maximum thickness of ice has been noted over the last 60 years•A disappearance of ice phenomena occurs during increases in westerly runoff•A lack of ice phenomena occurs during warm periods during th...
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Published in: | Oceanologia 2024-04, Vol.66 (2), p.153-166 |
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Main Authors: | , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites |
Online Access: | Get full text |
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Summary: | •For coastal lakes, a constant decrease in the number of days with ice is observed•A decrease in the maximum thickness of ice has been noted over the last 60 years•A disappearance of ice phenomena occurs during increases in westerly runoff•A lack of ice phenomena occurs during warm periods during the ice season•In addition to NAO, other factors strengthen ice phenomena
The paper represents an attempt to understand the impacts produced by the North Atlantic Oscillation on the ice cover regime of the largest coastal lake in Poland situated in the northern part of the country. The purpose of the study was to estimate the impact of the North Atlantic Oscillation on selected ice cover parameters. The study also attempts to examine other factors that may affect its significant impact on observed changes in the climate. Water temperature data are used to assess temperature conditions in aqueous ecosystems as well as determine the heat absorption capacity of these systems. This allows one to then determine cooling rates in the event of ice cover formation. The data analysis provided in the paper focuses on selected characteristics of ice cover conditions (i.e. dependent variables) including the number of days with ice and maximum ice thickness in relation to NAO index changes (i.e. independent variables) for the reference period 1960/61–2009/10. In addition, the paper divides the studied period into 10-year subperiods in order to capture the weakest and strongest phases of NAO and assess the extent to which they affect the duration of ice cover. A large increase in the mean air temperature (1.8°C) occurred in the years 1960–2010. Trendline analysis indicates that the number of days with ice cover declined by about 60 days and the maximum thickness of ice cover decreased by about 10 cm. Oceanographic research employs satellite image data in order to accurately assess human impact. Therefore, ice cover forecasts generated for consecutive winter seasons may become an important tool in this type of assessment. |
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ISSN: | 0078-3234 |
DOI: | 10.1016/j.oceano.2023.10.004 |