Nongrowing season methane emissions–a significant component of annual emissions across northern ecosystems

• Published in: Global Change Biology
• Main Authors: Treat, Claire C., Bloom, A. Anthony, Marushchak, Maija E.
• Other Authors: Biotieteiden ja Ympäristön Tutkimuksen Toimikunta, Division of Arctic Sciences, Jet Propulsion Laboratory, Erzincan Üniversitesi, National Science Foundation, National Aeronautics and Space Administration
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2018
• Subjects: permafrost; Tundra
• Online Access: http://dx.doi.org/10.1111/gcb.14137; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fgcb.14137; https://onlinelibrary.wiley.com/doi/pdf/10.1111/gcb.14137; https://onlinelibrary.wiley.com/doi/full-xml/10.1111/gcb.14137; https://onlinelibrary.wiley.com/doi/am-pdf/10.1111/gcb.14137

Abstract Wetlands are the single largest natural source of atmospheric methane (CH 4 ), a greenhouse gas, and occur extensively in the northern hemisphere. Large discrepancies remain between “bottom‐up” and “top‐down” estimates of northern CH 4 emissions. To explore whether these discrepancies are due to poor representation of nongrowing season CH 4 emissions, we synthesized nongrowing season and annual CH 4 flux measurements from temperate, boreal, and tundra wetlands and uplands. Median nongrowing season wetland emissions ranged from 0.9 g/m 2 in bogs to 5.2 g/m 2 in marshes and were dependent on moisture, vegetation, and permafrost. Annual wetland emissions ranged from 0.9 g m −2 year −1 in tundra bogs to 78 g m −2 year −1 in temperate marshes. Uplands varied from CH 4 sinks to CH 4 sources with a median annual flux of 0.0 ± 0.2 g m −2 year −1 . The measured fraction of annual CH 4 emissions during the nongrowing season (observed: 13% to 47%) was significantly larger than that was predicted by two process‐based model ensembles, especially between 40° and 60°N (modeled: 4% to 17%). Constraining the model ensembles with the measured nongrowing fraction increased total nongrowing season and annual CH 4 emissions. Using this constraint, the modeled nongrowing season wetland CH 4 flux from >40° north was 6.1 ± 1.5 Tg/year, three times greater than the nongrowing season emissions of the unconstrained model ensemble. The annual wetland CH 4 flux was 37 ± 7 Tg/year from the data‐constrained model ensemble, 25% larger than the unconstrained ensemble. Considering nongrowing season processes is critical for accurately estimating CH 4 emissions from high‐latitude ecosystems, and necessary for constraining the role of wetland emissions in a warming climate.