Greenhouse gas emission and storage in a small shallow lake
Small lakes are likely to show considerable temporal variability in greenhouse gas emissions given their transient stratification and short residence time. To determine the extent that CO 2 and CH 4 emission and storage depends on surface meteorology, we studied a shallow lake during 2 years with co...
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Published in | Hydrobiologia Vol. 757; no. 1; pp. 101 - 115 |
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Main Authors | , , |
Format | Journal Article |
Language | English |
Published |
Cham
Springer International Publishing
01.09.2015
Springer Springer Nature B.V |
Subjects | |
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Abstract | Small lakes are likely to show considerable temporal variability in greenhouse gas emissions given their transient stratification and short residence time. To determine the extent that CO
2
and CH
4
emission and storage depends on surface meteorology, we studied a shallow lake during 2 years with contrasting rainfall and thermal stratification. Gas fluxes were estimated with wind-based and surface renewal models and compared to direct measurements obtained with floating chambers. The assessment of greenhouse gases storage revealed that the lake gained CO
2
in association with rainfall in both the rainier (2011) and drier summer (2012). In 2011, stratification was less extensive and disrupted frequently. The lake was a source of CO
2
and CH
4
, and ebullition exceeded diffusive fluxes of CH
4
. In 2012, stratification was more persistent, the lake was a sink for CO
2
during dry periods, CO
2
and CH
4
accumulated in the hypolimnion later in the summer when rainfall increased, diffusive fluxes of CH
4
were similar to those in 2011 mid-summer and over four times higher during overturn. Ebullition was lower in the drier summer. Fluxes measured with chambers were closer to estimations from the surface renewal model and about two times values estimated with wind-based models. |
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AbstractList | Issue Title: THEMED SECTION: Ecology, Culture, and Management of Burbot Small lakes are likely to show considerable temporal variability in greenhouse gas emissions given their transient stratification and short residence time. To determine the extent that CO2 and CH4 emission and storage depends on surface meteorology, we studied a shallow lake during 2 years with contrasting rainfall and thermal stratification. Gas fluxes were estimated with wind-based and surface renewal models and compared to direct measurements obtained with floating chambers. The assessment of greenhouse gases storage revealed that the lake gained CO2 in association with rainfall in both the rainier (2011) and drier summer (2012). In 2011, stratification was less extensive and disrupted frequently. The lake was a source of CO2 and CH4, and ebullition exceeded diffusive fluxes of CH4. In 2012, stratification was more persistent, the lake was a sink for CO2 during dry periods, CO2 and CH4 accumulated in the hypolimnion later in the summer when rainfall increased, diffusive fluxes of CH4 were similar to those in 2011 mid-summer and over four times higher during overturn. Ebullition was lower in the drier summer. Fluxes measured with chambers were closer to estimations from the surface renewal model and about two times values estimated with wind-based models. Small lakes are likely to show considerable temporal variability in greenhouse gas emissions given their transient stratification and short residence time. To determine the extent that CO 2 and CH 4 emission and storage depends on surface meteorology, we studied a shallow lake during 2 years with contrasting rainfall and thermal stratification. Gas fluxes were estimated with wind-based and surface renewal models and compared to direct measurements obtained with floating chambers. The assessment of greenhouse gases storage revealed that the lake gained CO 2 in association with rainfall in both the rainier (2011) and drier summer (2012). In 2011, stratification was less extensive and disrupted frequently. The lake was a source of CO 2 and CH 4 , and ebullition exceeded diffusive fluxes of CH 4 . In 2012, stratification was more persistent, the lake was a sink for CO 2 during dry periods, CO 2 and CH 4 accumulated in the hypolimnion later in the summer when rainfall increased, diffusive fluxes of CH 4 were similar to those in 2011 mid-summer and over four times higher during overturn. Ebullition was lower in the drier summer. Fluxes measured with chambers were closer to estimations from the surface renewal model and about two times values estimated with wind-based models. Small lakes are likely to show considerable temporal variability in greenhouse gas emissions given their transient stratification and short residence time. To determine the extent that CO sub(2) and CH sub(4) emission and storage depends on surface meteorology, we studied a shallow lake during 2 years with contrasting rainfall and thermal stratification. Gas fluxes were estimated with wind-based and surface renewal models and compared to direct measurements obtained with floating chambers. The assessment of greenhouse gases storage revealed that the lake gained CO sub(2) in association with rainfall in both the rainier (2011) and drier summer (2012). In 2011, stratification was less extensive and disrupted frequently. The lake was a source of CO sub(2) and CH sub(4), and ebullition exceeded diffusive fluxes of CH sub(4). In 2012, stratification was more persistent, the lake was a sink for CO sub(2) during dry periods, CO sub(2) and CH sub(4) accumulated in the hypolimnion later in the summer when rainfall increased, diffusive fluxes of CH sub(4) were similar to those in 2011 mid-summer and over four times higher during overturn. Ebullition was lower in the drier summer. Fluxes measured with chambers were closer to estimations from the surface renewal model and about two times values estimated with wind-based models. |
Audience | Academic |
Author | MacIntyre, S. Bartosiewicz, M. Laurion, I. |
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Copyright | Springer International Publishing Switzerland 2015 COPYRIGHT 2015 Springer |
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Keywords | Diffusive flux Storage Ebullition Gas transfer modeling Thermal stratification Weather variability Greenhouse gases Small lake |
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SubjectTerms | Air pollution Analysis Aquatic ecological zones Biomedical and Life Sciences Carbon dioxide Ecology Emissions Freshwater Freshwater & Marine Ecology Greenhouse gases Hypolimnion Lakes Life Sciences Methane Pollution control Primary Research Paper Rain Rainfall Sediments Thermal stratification Weather Zoology |
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Title | Greenhouse gas emission and storage in a small shallow lake |
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