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Methane fluxes from...
Methane fluxes from a small boreal lake measured with the eddy covariance method
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- Podgrajsek, Eva (författare)
- Uppsala universitet,Luft-, vatten- och landskapslära,Uppsala University, Sweden
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- Sahlée, Erik (författare)
- Uppsala universitet,Luft-, vatten- och landskapslära,Uppsala University, Sweden
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- Bastviken, David (författare)
- Linköpings universitet,Tema Miljöförändring,Filosofiska fakulteten
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- Natchimuthu, Sivakiruthika (författare)
- Linköpings universitet,Tema Miljöförändring,Filosofiska fakulteten
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- Kljun, N. (författare)
- Swansea Univ, Dept Geog, Singleton Pk, Swansea, W Glam, Wales,Swansea University, Wales
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- Chmiel, Hannah (författare)
- Uppsala universitet,Limnologi,Uppsala University, Sweden
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- Klemedtsson, Leif, 1953 (författare)
- Gothenburg University,Göteborgs universitet,Institutionen för geovetenskaper,Department of Earth Sciences,Univ Gothenburg, Dept Earth Sci, Gothenburg, Sweden,University of Gothenburg, Sweden
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- Rutgersson, Anna (författare)
- Uppsala universitet,Luft-, vatten- och landskapslära,Uppsala University, Sweden
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(creator_code:org_t)
- 2015-12-30
- 2016
- Engelska.
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Ingår i: Limnology and Oceanography. - : Wiley. - 0024-3590 .- 1939-5590. ; 61:Supplement 1
- Relaterad länk:
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https://cronfa.swan....
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https://liu.diva-por... (primary) (Raw object)
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https://gup.ub.gu.se...
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https://doi.org/10.1...
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https://urn.kb.se/re...
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https://urn.kb.se/re...
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Abstract
Ämnesord
Stäng
- Fluxes of methane, CH4, were measured with the eddy covariance (EC) method at a small boreal lake in Sweden. The mean CH4 flux during the growing season of 2013 was 20.1 nmol m(-2) s(-1) and the median flux was 16 nmol m(-2) s(-1) (corresponding to 1.7 mmol m(-2) d(-1) and 1.4 mmol m(-2) d(-1)). Monthly mean values of CH4 flux measured with the EC method were compared with fluxes measured with floating chambers (FC) and were in average 62% higher over the whole study period. The difference was greatest in April partly because EC, but not FC, accounted for fluxes due to ice melt and a subsequent lake mixing event. A footprint analysis revealed that the EC footprint included primarily the shallow side of the lake with a major inlet. This inlet harbors emergent macrophytes that can mediate high CH4 fluxes. The difference between measured EC and FC fluxes can hence be explained by different footprint areas, where the EC system sees the part of the lake presumably releasing higher amounts of CH4. EC also provides more frequent measurements than FC and hence more likely captures ebullition events. This study shows that small lakes have CH4 fluxes that are highly variable in time and space. Based on our findings we suggest to measure CH4 fluxes from lakes as continuously as possible and to aim for covering as much of the lakes surface as possible, independently of the selected measuring technique.
Ämnesord
- NATURVETENSKAP -- Geovetenskap och miljövetenskap -- Geologi (hsv//swe)
- NATURAL SCIENCES -- Earth and Related Environmental Sciences -- Geology (hsv//eng)
- NATURVETENSKAP -- Geovetenskap och miljövetenskap -- Meteorologi och atmosfärforskning (hsv//swe)
- NATURAL SCIENCES -- Earth and Related Environmental Sciences -- Meteorology and Atmospheric Sciences (hsv//eng)
- NATURVETENSKAP -- Geovetenskap och miljövetenskap -- Multidisciplinär geovetenskap (hsv//swe)
- NATURAL SCIENCES -- Earth and Related Environmental Sciences -- Geosciences, Multidisciplinary (hsv//eng)
- NATURVETENSKAP -- Geovetenskap och miljövetenskap -- Naturgeografi (hsv//swe)
- NATURAL SCIENCES -- Earth and Related Environmental Sciences -- Physical Geography (hsv//eng)
Nyckelord
- greenhouse-gas emissions
- high-latitude lakes
- carbon-dioxide
- water-vapor
- ice melt
- exchange
- co2
- parameterization
- convection
- dynamics
- Marine & Freshwater Biology
- Oceanography
Publikations- och innehållstyp
- ref (ämneskategori)
- art (ämneskategori)
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