Reasons and patterns of spatio-temporal variability of methane emission from the Mozhaysk reservoir in summer period

Anthropogenic reservoirs are not only sources of clean energy, flow regulators, recreational and food resources, but also sources of greenhouse gases such as methane. The studies presented in this work, done on a well-studied low-flowing valley reservoir mainly in the summer, when the greatest varia...

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Main Authors: Lomov Viktor, Grechushnikova Maria, Kazantsev Vladimir, Repina Irina
Format: Article
Language:English
Published: EDP Sciences 2020-01-01
Series:E3S Web of Conferences
Online Access:https://www.e3s-conferences.org/articles/e3sconf/pdf/2020/23/e3sconf_vc2020_03010.pdf
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spelling doaj-9d19e3257fb044bbb23e40ba759f5a322021-04-02T11:32:54ZengEDP SciencesE3S Web of Conferences2267-12422020-01-011630301010.1051/e3sconf/202016303010e3sconf_vc2020_03010Reasons and patterns of spatio-temporal variability of methane emission from the Mozhaysk reservoir in summer periodLomov Viktor0Grechushnikova MariaKazantsev Vladimir1Repina Irina2Moscow State University, Faculty of Geography, Hydrology DepartmentInstitute of Atmosphere Physics Russian Academy of ScienceInstitute of Atmosphere Physics Russian Academy of ScienceAnthropogenic reservoirs are not only sources of clean energy, flow regulators, recreational and food resources, but also sources of greenhouse gases such as methane. The studies presented in this work, done on a well-studied low-flowing valley reservoir mainly in the summer, when the greatest variability of methane fluxes was observe. Depending on synoptic conditions, the temporal variability of methane fluxes varies greatly. Methane fluxes increase during the summer period and huge methane emissions observed before the autumn mixing stage. Emissions can occur during the destruction of temperature stratification, as a result of stormy weather. With such emissions, methane fluxes into the atmosphere can reach about 20 mgC*m-2*d-1, which is higher than the emission during convection. Revealing the patterns of spatio-temporal distribution of methane fluxes will help to determine the contribution of water bodies (in particular reservoirs) to the total methane budget of the atmosphere more accurately.https://www.e3s-conferences.org/articles/e3sconf/pdf/2020/23/e3sconf_vc2020_03010.pdf
collection DOAJ
language English
format Article
sources DOAJ
author Lomov Viktor
Grechushnikova Maria
Kazantsev Vladimir
Repina Irina
spellingShingle Lomov Viktor
Grechushnikova Maria
Kazantsev Vladimir
Repina Irina
Reasons and patterns of spatio-temporal variability of methane emission from the Mozhaysk reservoir in summer period
E3S Web of Conferences
author_facet Lomov Viktor
Grechushnikova Maria
Kazantsev Vladimir
Repina Irina
author_sort Lomov Viktor
title Reasons and patterns of spatio-temporal variability of methane emission from the Mozhaysk reservoir in summer period
title_short Reasons and patterns of spatio-temporal variability of methane emission from the Mozhaysk reservoir in summer period
title_full Reasons and patterns of spatio-temporal variability of methane emission from the Mozhaysk reservoir in summer period
title_fullStr Reasons and patterns of spatio-temporal variability of methane emission from the Mozhaysk reservoir in summer period
title_full_unstemmed Reasons and patterns of spatio-temporal variability of methane emission from the Mozhaysk reservoir in summer period
title_sort reasons and patterns of spatio-temporal variability of methane emission from the mozhaysk reservoir in summer period
publisher EDP Sciences
series E3S Web of Conferences
issn 2267-1242
publishDate 2020-01-01
description Anthropogenic reservoirs are not only sources of clean energy, flow regulators, recreational and food resources, but also sources of greenhouse gases such as methane. The studies presented in this work, done on a well-studied low-flowing valley reservoir mainly in the summer, when the greatest variability of methane fluxes was observe. Depending on synoptic conditions, the temporal variability of methane fluxes varies greatly. Methane fluxes increase during the summer period and huge methane emissions observed before the autumn mixing stage. Emissions can occur during the destruction of temperature stratification, as a result of stormy weather. With such emissions, methane fluxes into the atmosphere can reach about 20 mgC*m-2*d-1, which is higher than the emission during convection. Revealing the patterns of spatio-temporal distribution of methane fluxes will help to determine the contribution of water bodies (in particular reservoirs) to the total methane budget of the atmosphere more accurately.
url https://www.e3s-conferences.org/articles/e3sconf/pdf/2020/23/e3sconf_vc2020_03010.pdf
work_keys_str_mv AT lomovviktor reasonsandpatternsofspatiotemporalvariabilityofmethaneemissionfromthemozhayskreservoirinsummerperiod
AT grechushnikovamaria reasonsandpatternsofspatiotemporalvariabilityofmethaneemissionfromthemozhayskreservoirinsummerperiod
AT kazantsevvladimir reasonsandpatternsofspatiotemporalvariabilityofmethaneemissionfromthemozhayskreservoirinsummerperiod
AT repinairina reasonsandpatternsofspatiotemporalvariabilityofmethaneemissionfromthemozhayskreservoirinsummerperiod
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