Item talk:Q268488
From geokb
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"name": "Evidence for non-steady-state carbon emissions from snow-scoured alpine tundra",
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"abstract": "High-latitude warming is capable of accelerating permafrost degradation and the decomposition of previously frozen carbon. The existence of an analogous high-altitude feedback, however, has yet to be directly evaluated. We address this knowledge gap by coupling a radiocarbon-based model to 7 years (2008\u20132014) of continuous eddy covariance data from a snow-scoured alpine tundra meadow in Colorado, USA, where solifluction lobes are associated with discontinuous permafrost. On average, the ecosystem was a net annual source of 232\u2009\u00b1\u200954\u2009g\u2009C\u2009m\u22122\u00a0(mean\u2009\u00b1\u20091 standard deviation) to the atmosphere, and respiration of relatively radiocarbon-depleted (i.e., older) substrate contributes to carbon emissions during the winter. Given that alpine soils with permafrost occupy 3.6\u2009\u00d7\u2009106\u00a0km2\u00a0land area and are estimated to contain 66.3 Pg of soil organic carbon (4.5% of the global pool), this scenario has global implications for the mountain carbon balance and corresponding resource allocation to lower elevations.",
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