Methane Dynamics Associated with Tidal Processes in the Lower Columbia River
Tidally varying methane (CH₄) concentrations in estuaries may arise from physical advection and by chemical effects tied to varying exposure to salinity. An investigation of spatial and temporal variability in water-column CH₄ was conducted in the lower Columbia River using shipboard surveys and tim...
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Published in | Estuaries and coasts Vol. 42; no. 5; pp. 1249 - 1264 |
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Main Authors | , , , |
Format | Journal Article |
Language | English |
Published |
New York
Springer Science + Business Media
01.07.2019
Springer US Springer Nature B.V |
Subjects | |
Online Access | Get full text |
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Abstract | Tidally varying methane (CH₄) concentrations in estuaries may arise from physical advection and by chemical effects tied to varying exposure to salinity. An investigation of spatial and temporal variability in water-column CH₄ was conducted in the lower Columbia River using shipboard surveys and time series data from fixed stations. Peaks in CH₄ coincided with ebb tides at multiple sites located along the flank of the estuary adjacent to tidal flats and wetlands. High-resolution measurements taken at the outflow of a shallow lateral bay revealed that these CH₄ peaks were positively related to tidal amplitude when the lateral bay was exposed exclusively to freshwater over the tide cycle; in contrast, this relationship was inversed when brackish waters were involved. A positive relationship between tidal amplitude and CH₄ is consistent with a mechanism of tidal pumping from bottom sediments in the bay. In the presence of saltwater, however, a higher-than-expected flux of CH₄ could occur via suppression of removal processes such as biological oxidation. We present a conceptual model of tidal pumping modified by diurnal inequality in tidal amplitude and effects of salinity on sediment CH₄ oxidation to explain CH₄ variability on tidal to seasonal time-scales. The combined influences of tides and salinity likely affect CH₄ emissions in estuaries worldwide, making sea level rise and estuarine geomorphological change relevant factors for consideration when accounting for estuarine contributions to global methane budgets. |
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AbstractList | Tidally varying methane (CH4) concentrations in estuaries may arise from physical advection and by chemical effects tied to varying exposure to salinity. An investigation of spatial and temporal variability in water-column CH4 was conducted in the lower Columbia River using shipboard surveys and time series data from fixed stations. Peaks in CH4 coincided with ebb tides at multiple sites located along the flank of the estuary adjacent to tidal flats and wetlands. High-resolution measurements taken at the outflow of a shallow lateral bay revealed that these CH4 peaks were positively related to tidal amplitude when the lateral bay was exposed exclusively to freshwater over the tide cycle; in contrast, this relationship was inversed when brackish waters were involved. A positive relationship between tidal amplitude and CH4 is consistent with a mechanism of tidal pumping from bottom sediments in the bay. In the presence of saltwater, however, a higher-than-expected flux of CH4 could occur via suppression of removal processes such as biological oxidation. We present a conceptual model of tidal pumping modified by diurnal inequality in tidal amplitude and effects of salinity on sediment CH4 oxidation to explain CH4 variability on tidal to seasonal time-scales. The combined influences of tides and salinity likely affect CH4 emissions in estuaries worldwide, making sea level rise and estuarine geomorphological change relevant factors for consideration when accounting for estuarine contributions to global methane budgets. Tidally varying methane (CH₄) concentrations in estuaries may arise from physical advection and by chemical effects tied to varying exposure to salinity. An investigation of spatial and temporal variability in water-column CH₄ was conducted in the lower Columbia River using shipboard surveys and time series data from fixed stations. Peaks in CH₄ coincided with ebb tides at multiple sites located along the flank of the estuary adjacent to tidal flats and wetlands. High-resolution measurements taken at the outflow of a shallow lateral bay revealed that these CH₄ peaks were positively related to tidal amplitude when the lateral bay was exposed exclusively to freshwater over the tide cycle; in contrast, this relationship was inversed when brackish waters were involved. A positive relationship between tidal amplitude and CH₄ is consistent with a mechanism of tidal pumping from bottom sediments in the bay. In the presence of saltwater, however, a higher-than-expected flux of CH₄ could occur via suppression of removal processes such as biological oxidation. We present a conceptual model of tidal pumping modified by diurnal inequality in tidal amplitude and effects of salinity on sediment CH₄ oxidation to explain CH₄ variability on tidal to seasonal time-scales. The combined influences of tides and salinity likely affect CH₄ emissions in estuaries worldwide, making sea level rise and estuarine geomorphological change relevant factors for consideration when accounting for estuarine contributions to global methane budgets. Tidally varying methane (CH 4 ) concentrations in estuaries may arise from physical advection and by chemical effects tied to varying exposure to salinity. An investigation of spatial and temporal variability in water-column CH 4 was conducted in the lower Columbia River using shipboard surveys and time series data from fixed stations. Peaks in CH 4 coincided with ebb tides at multiple sites located along the flank of the estuary adjacent to tidal flats and wetlands. High-resolution measurements taken at the outflow of a shallow lateral bay revealed that these CH 4 peaks were positively related to tidal amplitude when the lateral bay was exposed exclusively to freshwater over the tide cycle; in contrast, this relationship was inversed when brackish waters were involved. A positive relationship between tidal amplitude and CH 4 is consistent with a mechanism of tidal pumping from bottom sediments in the bay. In the presence of saltwater, however, a higher-than-expected flux of CH 4 could occur via suppression of removal processes such as biological oxidation. We present a conceptual model of tidal pumping modified by diurnal inequality in tidal amplitude and effects of salinity on sediment CH 4 oxidation to explain CH 4 variability on tidal to seasonal time-scales. The combined influences of tides and salinity likely affect CH 4 emissions in estuaries worldwide, making sea level rise and estuarine geomorphological change relevant factors for consideration when accounting for estuarine contributions to global methane budgets. |
Author | Wolhowe, Matthew Pfeiffer-Herbert, Anna S. Peterson, Tawnya D. Prahl, Fredrick G. |
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CitedBy_id | crossref_primary_10_5194_bg_17_5809_2020 crossref_primary_10_1016_j_watres_2023_121012 crossref_primary_10_1016_j_ecss_2022_107786 |
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Copyright | Coastal and Estuarine Research Federation 2019 Estuaries and Coasts is a copyright of Springer, (2019). All Rights Reserved. |
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SubjectTerms | Amplitude Amplitudes Biological activity Biological oxidation Bottom sediments Brackishwater environment Chemical effects Coastal Sciences Diurnal Earth and Environmental Science Ebb tides Ecology Environment Environmental Management Estuaries Estuarine dynamics Fixed stations Freshwater Freshwater & Marine Ecology Geomorphology Inland water environment Methane Organic chemistry ORIGINAL PAPERS Outflow Oxidation Pumping Rivers Saline water Salinity Salinity effects Sea level Sea level rise Sediments Spatial distribution Surveys Temporal variations Tidal amplitude Tidal flats Tides Variability Water and Health Water circulation |
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Title | Methane Dynamics Associated with Tidal Processes in the Lower Columbia River |
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