Greenhouse gas flux from headwater streams in New Hampshire, USA: Patterns and drivers. (20th June 2016)

• Record Type: Journal Article
• Authors: Schade, John D.; Bailio, Jason; McDowell, William H.
• Other Names: Wickland Kimberly guestEditor.; Hamdan Leila guestEditor.
• Is Part Of: Limnology and oceanography. Volume 61(2016)Supplement 1
• Page Start: S165
• Page End: S174
• Publication Date: 2016-06-20
• Subjects: Limnology -- Periodicals; Oceanography -- Periodicals; Océanographie; Limnologie; Limnology; Oceanography; Computer network resources; Périodique électronique (Descripteur de forme); Ressource Internet (Descripteur de forme); Periodicals; 551.4805
• DOI: 10.1002/lno.10337
• Languages: English
• ISSNs: 0024-3590

Abstract

Abstract: Freshwater ecosystems can be considerable sources of greenhouse gases (GHG), however, much uncertainty remains in global estimates and understanding of drivers of these emissions. Furthermore, headwater streams have received insufficient attention and may contribute disproportionately to global GHG flux. Our objective was to quantify carbon dioxide (CO2 ), methane (CH4 ), and nitrous oxide (N2 O) flux and assess the impact of changes in dissolved organic carbon (DOC) and NO3 concentrations on GHG flux in three streams in the Lamprey River watershed in New Hampshire, U.S.A., that contrast in surface water DOC: NO3 . We measured DOC, NO3 and dissolved gas partial pressures and estimated gas flux in surface waters monthly from May 2011 to April 2012. We found higher GHG partial pressures and fluxes in the two streams with high DOC concentrations. The stream with high DOC and high NO3 showed high N2 O and low CH4 flux, while the high DOC, low NO3 stream showed high CH4 and low N2 O flux. Our results support a model in which C inputs drive total GHG production, while NO3 input regulates the relative importance of CH4 and N2 O, likely by suppressing methanogenesis and stimulating denitrification. Results suggest streams in this region are small sources of CO2, but potentially important sources of CH4 and N2 O. Since CH4 and N2 O are more powerful than CO2 at trapping heat in the atmosphere, freshwater emissions of these gases have the potential to partially offset climate benefits of terrestrial carbon sinks, a possibility that has not been sufficiently incorporated into climate models.