Effect of permafrost thaw on methane and carbon dioxide exchange in two western Alaska peatlands

Methane (CH 4) causes about 20% of greenhouse gas radiative forcing despite its relatively short lifetime (~10 y) and low concentration (1800 ppb) in the atmosphere. Wetlands are the largest natural source of CH 4, amounting to 22% of CH 4 production globally, with emission of CH 4-C by both diffusi...

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Bibliographic Details
Main Author: Johnston, Carmel Eliise
Other Authors: Chairperson, Graduate Committee: Stephanie A. Ewing, Stephanie A. Ewing, Jennifer W. Harden, Paul C. Stoy, Ruth K. Varner, Kimberly P. Wickland, Joshua Koch, Christopher Fuller and Mark T. Jorgenson were co-authors of the article, '2.0 effect of permafrost thaw on CO 2 and CH 4 exchange in a western Alaska peatland chronosequence' submitted to the journal 'Environmental research letters' which is contained within this thesis., Stephanie A. Ewing, Merritt R. Turetsky, Jennifer W. Harden, A. David McGuire and Miriam Jones were co-authors of the article, '3.0 effect of recent permafrost thaw on the spatial distribution of CO 2 and CH 4 exchange in a western Alaska peatland' submitted to the journal 'Environmental research letters' which is contained within this thesis.
Format: Thesis
Language:English
Published: Montana State University - Bozeman, College of Agriculture 2013
Subjects:
Online Access:https://scholarworks.montana.edu/xmlui/handle/1/9099