Acclimation of ecosystem CO2 exchange in the Alaskan Arctic in response to decadal climate warming

By W. Oechel, G. Vourlitis, S. J. Hastings, R. Zulueta, L. Hinzman, D. Kane. Nature, 2000

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Citations in the corpus

Biotic controls on CO2 and CH4 exchange in wetlands – a closed environment study (2003, background): “Northern peatlands and wet tundra regions contain large amounts of stored organic carbon, and their potential for exchange of greenhouse gases (CO2 ,C H 4) with the atmosphere is therefore great (Gorham 1991; Oechel et al. 1993, 2000; Christensen et al. 1999).”
Geophysical Applications of Vegetation Modeling (2001, background): “Recent studies have proposed that high-latitude vegetation will gain in productivity due to increased nutrient availability as a result of warming in the Arctic [Chapin et al., 1995b; Melillo et al., 1993; Oechel et al., 1994; Oechel et al., 2000].”
The response of two Glomus mycorrhizal fungi and a fine endophyte to elevated atmospheric CO2, soil warming and drought (2004, background): “Most of the research investigating the consequences of future climate change, and concomitant increasing atmospheric CO2, on terrestrial ecosystems has been focused on the vegetation (e.g. Oechel et al., 2000), and in particular on the aboveground component.”
Inter-annual carbon dioxide uptake of a wet sedge tundra ecosystem in the Arctic (2003, background): “Also, the highlatitude warming is expected to increase greenhousegas emission, which can accelerate global warming (Oechel and Vourlitis, 1997; Oechel et al., 2000).”
Linking flux network measurements to continental scale simulations: ecosystem carbon dioxide exchange capacity under non‐water‐stressed conditions (2007, neutral): “(2003), Oechel et al. (2000)”
Long-term sensitivity of soil carbon turnover to warming (2005, background): “In soil warming experiments, the initially increased carbon dioxide efflux returns to pre-warming rates within one to three year”
Higher northern latitude normalized difference vegetation index and growing season trends from 1982 to 1999 (2001, background): “This is consistent with the reported increased winter and spring temperatures (Rigor et al. 2000; Hansen et al. 1999; Oechel et al. 2000 ), a reduced extent of snow cover in the Northern Hemisphere (Groisman et al. 1994), reductions in arctic sea ice (Chapman and Walsh 1993; Parkinson et al. 1999),”
Temperature sensitivity of soil organic matter decomposition—what do we know? (2009, background): “The decay rate of the labile SOM is very temperaturesensitive, but not the decay rate of stable SOM (Bradford et al. 2008; Eliasson et al. 2005; Liski et al. 1999; Luo et al. 2001; Melillo et al. 2002; Oechel et al. 2000; Trumbore et al. 1996).”
Microbial biomass, functional capacity, and community structure after 12 years of soil warming (2008, background): “However, this stimulatory effect significantly decreased after 5–6 years of warming and there was no response to heating between years 7 and 12. Similar results have been observed by others ( Oechel et al., 2000; Luo et al., 2001).”
Winter Biological Processes Could Help Convert Arctic Tundra to Shrubland (2005, background): “With the 18 BioScience • January 2005 / Vol. 55 No. 1 production of more woody material and the change in soil moisture levels due to shading, short- and long-term shifts in net carbon exchange and carbon storage would be set in motion (Oechel et al. 2000).”
Integrating microbial ecology into ecosystem models: challenges and priorities (2012, background): “However, in field-based studies, warming-induced increases in soil respiration rates can be short-lived, returning to pre-warming levels within a decade or so (Jarvis and Linder 2000; Luo et al. 2001; Melillo et al. 2002; Oechel et al. 2000; Rustad et al. 2001).”