Warming and drying effects on tundra carbon balance
Changes in permafrost carbon (C) storage are expected to be one of the most important and rapid feedbacks from terrestrial ecosystems to atmospheric CO2 concentrations. If the availability of permafrost C increases in a warmer and drier climate, as predicted for the study region, these systems may s...
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Arctic Data Center
2015
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Online Access: | https://search.dataone.org/view/urn:uuid:4fb67d3a-0c98-48d5-b851-dc49a21f263f |