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Methane emissions from tundra environments in the Yukon‐Kuskokwim delta, Alaska
324
Citations
39
References
1992
Year
Organic GeochemistryBiogeochemistryAverage FluxesEngineeringTerrestrial EcosystemMicrometeorologyGreenhouse Gas EmissionTerrestrial EcologyWet Meadow TundraForest MeteorologyBiogeochemical ProcessEnclosure TechniquesEarth ScienceCoal Bed MethaneClimate ChangeTundra Environments
Over a 6‐week period from July 3 to August 10, 1988, we made measurements of the flux of methane by enclosure techniques from major tundra environments in the Yukon‐Kuskokwim Delta of Alaska (60°45′N). Emissions from wet meadow tundra averaged 144 ± 31 mg CH 4 /m 2 /d and ranged from 15.6 to 426 mg CH 4 /m 2 /d, varying with soil moisture and temperature. Flux from the drier upland tundra was approximately 2 orders of magnitude lower and averaged 2.3 ± 1.1 mg CH 4 /m 2 /d. Consumption of ambient levels of methane was sporadically measured at these drier sites, and emissions ranged between −2.1 and 18.1 mg CH 4 /m 2 /d. Tundra lakes emit methane from the open water surface as well as from fringing aquatic vegetation. The presence of vegetation significantly enhanced flux over open water rates. Average fluxes from a variety of sites with vegetation ranged between 62.7 and 153.5 mg CH 4 /m 2 /d. Calculated diffusive fluxes from open water varied with lake size, the large lakes emitting 3.8 mg CH 4 /m 2 /d and small lakes emitting an average of 77 mg CH 4 /m 2 /d. An updated estimate of global emissions from tundra indicates an annual flux of approximately 11 ± 3 Tg CH 4 .
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