Detailed Patterns of Methane Distribution in the German Bight

Although methane is a widely studied greenhouse gas, uncertainties remain with respect to the factors controlling its distribution and diffusive flux into the atmosphere, especially in highly dynamic coastal waters. In the southern North Sea, the Elbe and Weser rivers are two major tributaries contr...

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Main Authors: Ingeborg Bussmann, Holger Brix, Götz Flöser, Uta Ködel, Philipp Fischer
Format: Article
Language:English
Published: Frontiers Media S.A. 2021-09-01
Series:Frontiers in Marine Science
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/fmars.2021.728308/full
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spelling doaj-f017af925bc240e89aa2d4913ac8e54a2021-09-17T05:35:46ZengFrontiers Media S.A.Frontiers in Marine Science2296-77452021-09-01810.3389/fmars.2021.728308728308Detailed Patterns of Methane Distribution in the German BightIngeborg Bussmann0Holger Brix1Götz Flöser2Uta Ködel3Philipp Fischer4Departments of Marine Geochemistry and Shelf Sea System Ecology, Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung, Bremerhaven, GermanyInstitute of Coastal Ocean Dynamics, Helmholtz-Zentrum Hereon, Geesthacht, GermanyInstitute of Coastal Ocean Dynamics, Helmholtz-Zentrum Hereon, Geesthacht, GermanyDepartment Monitoring and Exploration Technologies, Helmholtz-Zentrum für Umweltforschung, Leipzig, GermanyLogistics and Research Platfomrs and Shelf Sea System Ecology, Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung, Helgoland, GermanyAlthough methane is a widely studied greenhouse gas, uncertainties remain with respect to the factors controlling its distribution and diffusive flux into the atmosphere, especially in highly dynamic coastal waters. In the southern North Sea, the Elbe and Weser rivers are two major tributaries contributing to the overall methane budget of the southern German Bight. In June 2019, we continuously measured methane and basic hydrographic parameters at a high temporal and spatial resolution (one measurement per minute every 200–300 m) on a transect between Cuxhaven and Helgoland. These measurements revealed that the overall driver of the coastal methane distribution is the dilution of riverine methane-rich water with methane-poor marine water. For both the Elbe and Weser, we determined an input concentration of 40–50 nmol/L compared to only 5 nmol/L in the marine area. Accordingly, we observed a comparatively steady dilution pattern of methane concentration toward the marine realm. Moreover, small-scale anomalous patterns with unexpectedly higher dissolved methane concentrations were discovered at certain sites and times. These patterns were associated with the highly significant correlations of methane with oxygen or turbidity. However, these local anomalies were not consistent over time (days, months). The calculated diffusive methane flux from the water into the atmosphere revealed local values approximately 3.5 times higher than background values (median of 36 and 128 μmol m–2 d–1). We evaluate that this occurred because of a combination of increasing wind speed and increasing methane concentration at those times and locations. Hence, our results demonstrate that improved temporal and spatial resolution of methane measurements can provide a more accurate estimation and, consequently, a more functional understanding of the temporal and spatial dynamics of the coastal methane flux.https://www.frontiersin.org/articles/10.3389/fmars.2021.728308/fulldissolved methaneNorth Seahigh temporal resolutionhigh spatial resolutiondiffusive methane flux
collection DOAJ
language English
format Article
sources DOAJ
author Ingeborg Bussmann
Holger Brix
Götz Flöser
Uta Ködel
Philipp Fischer
spellingShingle Ingeborg Bussmann
Holger Brix
Götz Flöser
Uta Ködel
Philipp Fischer
Detailed Patterns of Methane Distribution in the German Bight
Frontiers in Marine Science
dissolved methane
North Sea
high temporal resolution
high spatial resolution
diffusive methane flux
author_facet Ingeborg Bussmann
Holger Brix
Götz Flöser
Uta Ködel
Philipp Fischer
author_sort Ingeborg Bussmann
title Detailed Patterns of Methane Distribution in the German Bight
title_short Detailed Patterns of Methane Distribution in the German Bight
title_full Detailed Patterns of Methane Distribution in the German Bight
title_fullStr Detailed Patterns of Methane Distribution in the German Bight
title_full_unstemmed Detailed Patterns of Methane Distribution in the German Bight
title_sort detailed patterns of methane distribution in the german bight
publisher Frontiers Media S.A.
series Frontiers in Marine Science
issn 2296-7745
publishDate 2021-09-01
description Although methane is a widely studied greenhouse gas, uncertainties remain with respect to the factors controlling its distribution and diffusive flux into the atmosphere, especially in highly dynamic coastal waters. In the southern North Sea, the Elbe and Weser rivers are two major tributaries contributing to the overall methane budget of the southern German Bight. In June 2019, we continuously measured methane and basic hydrographic parameters at a high temporal and spatial resolution (one measurement per minute every 200–300 m) on a transect between Cuxhaven and Helgoland. These measurements revealed that the overall driver of the coastal methane distribution is the dilution of riverine methane-rich water with methane-poor marine water. For both the Elbe and Weser, we determined an input concentration of 40–50 nmol/L compared to only 5 nmol/L in the marine area. Accordingly, we observed a comparatively steady dilution pattern of methane concentration toward the marine realm. Moreover, small-scale anomalous patterns with unexpectedly higher dissolved methane concentrations were discovered at certain sites and times. These patterns were associated with the highly significant correlations of methane with oxygen or turbidity. However, these local anomalies were not consistent over time (days, months). The calculated diffusive methane flux from the water into the atmosphere revealed local values approximately 3.5 times higher than background values (median of 36 and 128 μmol m–2 d–1). We evaluate that this occurred because of a combination of increasing wind speed and increasing methane concentration at those times and locations. Hence, our results demonstrate that improved temporal and spatial resolution of methane measurements can provide a more accurate estimation and, consequently, a more functional understanding of the temporal and spatial dynamics of the coastal methane flux.
topic dissolved methane
North Sea
high temporal resolution
high spatial resolution
diffusive methane flux
url https://www.frontiersin.org/articles/10.3389/fmars.2021.728308/full
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