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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2020-01-01
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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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