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• W2009641352 abstract "Factors controlling the flux of the radiatively important trace gas methane (CH 4 ) from boreal wetlands were examined at three sites along a moisture gradient from a treed low‐shrub bog to an open floating graminoid bog in Fairbanks, Alaska. In the summer of 1992 average static chamber flux measurements were −0.02, 71.5, and 289 mg CH 4 /m 2 /d in dry, wet, and floating mat communities, respectively. In contrast, the warmer, drier 1993 field season flux measurements were −0.02, 42.9 and 407 mg CH 4 /m 2 /d. The data indicate that despite net oxidation of CH 4 in the dry regions of the bog, the wetland is a net source of CH 4 , with fluxes ranging across three orders of magnitude between different plant communities. Comparison with water levels suggests that CH 4 flux is turned on and off by changes in site hydrology. In sites where sufficient moisture is present for methanogenesis to occur, CH 4 flux appears to be temperature limited, responding exponentially to soil temperature changes. The combined effects of hydrology and temperature create hot spots of CH 4 flux within boreal wetlands. The plant communities within Lemeta Bog respond differently to changes in temperature and moisture availability, creating both positive and negative feedbacks to potential global climate change." @default.
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• W2009641352 date "1996-06-01" @default.
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• W2009641352 title "Controls on CH₄flux from an Alaskan boreal wetland" @default.
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• W2009641352 doi "https://doi.org/10.1029/96gb00358" @default.
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