Trends in CO2exchange in a high Arctic tundra heath, 2000-2010
about
Net ecosystem exchange of CO2 with rapidly changing high Arctic landscapes.Warming of subarctic tundra increases emissions of all three important greenhouse gases - carbon dioxide, methane, and nitrous oxide.A synthesis of the arctic terrestrial and marine carbon cycles under pressure from a dwindling cryosphereSpatiotemporal variability in surface energy balance across tundra, snow and ice in GreenlandHotspots and key periods of Greenland climate change during the past six decades.Monitoring the multi-year carbon balance of a subarctic palsa mire with micrometeorological techniques.Long-Term Drainage Reduces CO2 Uptake and CH4 Emissions in a Siberian Permafrost EcosystemAnnual patterns and budget of CO2flux in an Arctic tussock tundra ecosystemTundra is a consistent source of CO2 at a site with progressive permafrost thaw during 6 years of chamber and eddy covariance measurements
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Trends in CO2exchange in a high Arctic tundra heath, 2000-2010
description
im April 2012 veröffentlichter wissenschaftlicher Artikel
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wetenschappelijk artikel
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наукова стаття, опублікована у квітні 2012
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name
Trends in CO2exchange in a high Arctic tundra heath, 2000-2010
@en
Trends in CO2exchange in a high Arctic tundra heath, 2000-2010
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type
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Trends in CO2exchange in a high Arctic tundra heath, 2000-2010
@en
Trends in CO2exchange in a high Arctic tundra heath, 2000-2010
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prefLabel
Trends in CO2exchange in a high Arctic tundra heath, 2000-2010
@en
Trends in CO2exchange in a high Arctic tundra heath, 2000-2010
@nl
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Trends in CO2exchange in a high Arctic tundra heath, 2000-2010
@en
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Charlotte Sigsgaard
Henrik Soegaard
Julie M. Falk
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10.1029/2011JG001901
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P577
2012-04-04T00:00:00Z