Measurement of the 13C isotopic signature of methane emissions from northern European wetlands. / Fisher, Rebecca; France, James; Lowry, David; Lanoiselle, Mathias; Brownlow, Rebecca; Pyle, John; Cain, Michelle; Warwick, Nicola; Skiba, Ute; Drewer, Julia; Dinsmore, Kerry; Leeson, Sarah; Bauguitte, Stephane; Wellpott, Axel; O'Shea, Sebastian; Allen, Grant; Gallagher, Martin; Pitt, Joseph; Percival, Carl; Bower, Keith; George, Charles; Hayman, Garry; Aalto, Tuula; Lohila, Annalea; Aurela, Mika; Laurila, Tuomas; Crill, Patrick; McCalley, Carmody; Nisbet, Euan.

In: Global Biogeochemical Cycles, Vol. 31, No. 3, 03.2017, p. 605–623.

Research output: Contribution to journalArticle

Published

Documents

  • John Pyle
  • Michelle Cain
  • Nicola Warwick
  • Ute Skiba
  • Julia Drewer
  • Kerry Dinsmore
  • Sarah Leeson
  • Stephane Bauguitte
  • Axel Wellpott
  • Sebastian O'Shea
  • Grant Allen
  • Martin Gallagher
  • Joseph Pitt
  • Carl Percival
  • Keith Bower
  • Charles George
  • Garry Hayman
  • Tuula Aalto
  • Annalea Lohila
  • Mika Aurela
  • Tuomas Laurila
  • Patrick Crill
  • Carmody McCalley

Abstract

Isotopic data provide powerful constraints on regional and global methane emissions and their source profiles. However, inverse modeling of spatially resolved methane flux is currently constrained by a lack of information on the variability of source isotopic signatures. In this study, isotopic signatures of emissions in the Fennoscandian Arctic have been determined in chambers over wetland, in the air 0.3 to 3m above the wetland surface and by aircraft sampling from 100m above wetlands up to the stratosphere. Overall, the methane flux to atmosphere has a coherent δ13C isotopic signature of -71±1‰, measured in situ on the ground in wetlands. This is in close agreement with δ13C isotopic signatures of local and regional methane increments measured by aircraft campaigns flying through air masses containing elevated methane mole fractions. In contrast, results from wetlands in Canadian boreal forest farther south gave isotopic signatures of -67±1‰. Wetland emissions dominate the local methane source measured over the European Arctic in summer. Chamber measurements demonstrate a highly variable methane flux and isotopic signature, but the results from air sampling within wetland areas show that emissions mix rapidly immediately above the wetland surface and methane emissions reaching the wider atmosphere do indeed have strongly coherent C isotope signatures. The study suggests that for boreal wetlands (>60°N) global and regional modeling can use an isotopic signature of -71‰ to apportion sources more accurately, but there is much need for further measurements over other wetlands regions to verify this.
Original languageEnglish
Pages (from-to)605–623
Number of pages19
JournalGlobal Biogeochemical Cycles
Volume31
Issue number3
Early online date31 Mar 2017
DOIs
Publication statusPublished - Mar 2017
This open access research output is licenced under a Creative Commons Attribution-NonCommercial-NoDerivs 3.0 Unported License.

ID: 27854978