ON FORECASTING LONG-TERM VARIATIONS OF WATER LEVEL IN LARGE LAKES

<p>The paper assesses the present-day state and long-term forecast of intrasecular oscillations of water level in large Eurasian lakes. The analysis of the North Atlantic climate change influence on the catchments hydrological regime of the Caspian Sea and Ladoga and Onega lakes was made on th...

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Main Authors: Tatiana Vyruchalkina, Nikolai Filatov, Nikolai Diansky, Anatoly Gusev
Format: Article
Language:English
Published: Karelian Research Centre of the Russian Academy of Sciences 2016-10-01
Series:Transactions of the Karelian Research Centre of the Russian Academy of Sciences
Subjects:
Online Access:http://journals.krc.karelia.ru/index.php/limnology/article/view/480
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author Tatiana Vyruchalkina
Nikolai Filatov
Nikolai Diansky
Anatoly Gusev
author_facet Tatiana Vyruchalkina
Nikolai Filatov
Nikolai Diansky
Anatoly Gusev
author_sort Tatiana Vyruchalkina
collection DOAJ
description <p>The paper assesses the present-day state and long-term forecast of intrasecular oscillations of water level in large Eurasian lakes. The analysis of the North Atlantic climate change influence on the catchments hydrological regime of the Caspian Sea and Ladoga and Onega lakes was made on the basis of the reanalysis data and numerical simulation results. The connection between some indexes of atmospheric and oceanic circulation describing climatic variability of the North Atlantic and Europe and hydrological regime of Volga and Neva rivers basins was estimated. The paper investigates the causal effects between climatic characteristics and catchments hydrological regime and the lakes water level. Several years’ time lag of hydrological regime (rivers runoff, the Caspian Sea level) response to changes in atmospheric circulation was shown. The dynamics of precipitation in the Caspian catchment correspond to changes in circulation indexes. Moisture transport from the Atlantic to the European part of Russia in the 21st century was estimated using the combined scenario of climate changes based on the hybrid of <em>greenhouse</em> and <em>cyclic</em> effects. The simulation results reveal possible decrease of moisture transport and atmospheric precipitation over the European part of Russia for the next 15-20 years resulting (with several years’ time lag) in the ongoing water level decrease in the Caspian Sea and Lake Ladoga. Moisture transport increase is expected from around 2035 to 2070, which will presumably lead to precipitation increase and water level rise in these water bodies.</p>
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spelling doaj.art-7ab35f5b8fe7406bace1e436961a86da2022-12-21T23:57:54ZengKarelian Research Centre of the Russian Academy of SciencesTransactions of the Karelian Research Centre of the Russian Academy of Sciences1997-32172312-45042016-10-01931610.17076/lim480290ON FORECASTING LONG-TERM VARIATIONS OF WATER LEVEL IN LARGE LAKESTatiana Vyruchalkina0Nikolai FilatovNikolai Diansky1Anatoly Gusev2Water Problems Institute, Russian Academy of SciencesInstitute of Numerical Mathematics, Russian Academy of SciencesInstitute of Numerical Mathematics, Russian Academy of Sciences<p>The paper assesses the present-day state and long-term forecast of intrasecular oscillations of water level in large Eurasian lakes. The analysis of the North Atlantic climate change influence on the catchments hydrological regime of the Caspian Sea and Ladoga and Onega lakes was made on the basis of the reanalysis data and numerical simulation results. The connection between some indexes of atmospheric and oceanic circulation describing climatic variability of the North Atlantic and Europe and hydrological regime of Volga and Neva rivers basins was estimated. The paper investigates the causal effects between climatic characteristics and catchments hydrological regime and the lakes water level. Several years’ time lag of hydrological regime (rivers runoff, the Caspian Sea level) response to changes in atmospheric circulation was shown. The dynamics of precipitation in the Caspian catchment correspond to changes in circulation indexes. Moisture transport from the Atlantic to the European part of Russia in the 21st century was estimated using the combined scenario of climate changes based on the hybrid of <em>greenhouse</em> and <em>cyclic</em> effects. The simulation results reveal possible decrease of moisture transport and atmospheric precipitation over the European part of Russia for the next 15-20 years resulting (with several years’ time lag) in the ongoing water level decrease in the Caspian Sea and Lake Ladoga. Moisture transport increase is expected from around 2035 to 2070, which will presumably lead to precipitation increase and water level rise in these water bodies.</p>http://journals.krc.karelia.ru/index.php/limnology/article/view/480forecastwater levellakesclimatevariability
spellingShingle Tatiana Vyruchalkina
Nikolai Filatov
Nikolai Diansky
Anatoly Gusev
ON FORECASTING LONG-TERM VARIATIONS OF WATER LEVEL IN LARGE LAKES
Transactions of the Karelian Research Centre of the Russian Academy of Sciences
forecast
water level
lakes
climate
variability
title ON FORECASTING LONG-TERM VARIATIONS OF WATER LEVEL IN LARGE LAKES
title_full ON FORECASTING LONG-TERM VARIATIONS OF WATER LEVEL IN LARGE LAKES
title_fullStr ON FORECASTING LONG-TERM VARIATIONS OF WATER LEVEL IN LARGE LAKES
title_full_unstemmed ON FORECASTING LONG-TERM VARIATIONS OF WATER LEVEL IN LARGE LAKES
title_short ON FORECASTING LONG-TERM VARIATIONS OF WATER LEVEL IN LARGE LAKES
title_sort on forecasting long term variations of water level in large lakes
topic forecast
water level
lakes
climate
variability
url http://journals.krc.karelia.ru/index.php/limnology/article/view/480
work_keys_str_mv AT tatianavyruchalkina onforecastinglongtermvariationsofwaterlevelinlargelakes
AT nikolaifilatov onforecastinglongtermvariationsofwaterlevelinlargelakes
AT nikolaidiansky onforecastinglongtermvariationsofwaterlevelinlargelakes
AT anatolygusev onforecastinglongtermvariationsofwaterlevelinlargelakes