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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Bibliographic Details
Main Author: Susan Natali
Format: Dataset
Language:unknown
Published: Arctic Data Center 2015
Subjects:
Online Access:https://search.dataone.org/view/urn:uuid:4fb67d3a-0c98-48d5-b851-dc49a21f263f