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WHAT IS GOING ON WITH INTRASECULAR WATER LEVEL FLUCTUATIONS IN THE GREAT LAKES OF EURASIA?
- Authors: Filatov N.N.1,2, Malinin V.N.3
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Affiliations:
- Northern Water Problems Institute, Karelian Research Centre
- Shirshov Institute of Oceanology, Russian Academy of Sciences
- Hydrometeorological University
- Issue: Vol 525, No 1 (2025)
- Pages: 167–172
- Section: LAND WATERS PROBLEMS
- Submitted: 26.12.2025
- Published: 15.11.2024
- URL: https://ogarev-online.ru/2686-7397/article/view/362871
- DOI: https://doi.org/10.7868/S303450652510195
- ID: 362871
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Abstract
In the paper discusses why the intrasecular fluctuations of the level of the great lakes of Eurasia differ so significantly. The paper addresses both the phenomenon of the lowest position of the Caspian water level over the entire the history of observations and the problems of regulation of the Lake Baikal level that have been discussed over the past several decades. The paper substantiates the causes of an essential difference in the intrasecular fluctuations and multidirectional trends in the level of Ladoga and Onego lakes that are part of a single water system. Discussed are the specific features in the variability of the level of the great Eurasian lakes amid the global climate warming, the mechanisms of the lake level variability and the possible ways of forecasting long-term changes in lake water level.
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About the authors
N. N. Filatov
Northern Water Problems Institute, Karelian Research Centre; Shirshov Institute of Oceanology, Russian Academy of Sciences
Email: nfilatov@rambler.ru
Corresponding Member of the RAS Petrozavodsk, Russia; Saint Petersburg, Russia
V. N. Malinin
Hydrometeorological UniversitySaint Petersburg, Russia
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