Filters: Categories: Publication (X) > Categories: Data (X) > partyWithName: McGuire, A. D. (X)
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Tags: Modeling,
Monitoring 3-Improve Permafrost Mapping,
and Monitoring
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Tags: P3b-Vegatation Productivity Changes Due to Temperature change
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Tags: Projecting Future States 3a-Future Vulnerability to Land use Change
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Tags: P2-Changes in Plant and Animal Species Due to Climate Change
Growing season CH4 fluxes were monitored over a two year period following the start of ecosystem-scale manipulations of water table position and surface soil temperatures in a moderate rich fen in interior Alaska. The largest CH4 fluxes occurred in plots that received both flooding (raised water table position) and soil warming, while the lowest fluxes occurred in unwarmed plots in the lowered water table treatment. A combination of treatment and soil hydroclimate variables explained more than 70% of the variation in ln-transformed CH4 fluxes, with mean daily water table position representing the strongest predictor. We used quantitative PCR of the -subunit of mcr operon to explore the influence of soil climate...
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Tags: Monitoring 2-Standardized Stream and Lake Information,
Monitoring 5-Physical Science
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Tags: R1-Vulnerability Forest Species and Communities to Climate Change
To determine the influence of fire and thermokarst in a boreal landscape, we investigated peat cores within and adjacent to a permafrost collapse feature on the Tanana River Floodplain of Interior Alaska. Radioisotope dating, diatom assemblages, plant macrofossils, charcoal fragments, and carbon and nitrogen content of the peat profile indicate ~600 years of vegetation succession with a transition from a terrestrial forest to a sedge-dominated wetland over 100 years ago, and to a Sphagnum-dominated peatland in approximately 1970. The shift from sedge to Sphagnum, and a decrease in the detrended tree-ring width index of black spruce trees adjacent to the collapse coincided with an increase in the growing season temperature...
To test the effects of altered hydrology on organic soil decomposition, we investigated CO2 and CH4 production potential of rich-fen peat (mean surface pH = 6.3) collected from a field water table manipulation experiment including control, raised and lowered water table treatments. Mean anaerobic CO2 production potential at 10 cm depth (14.1 ± 0.9 μmol C g−1 d−1) was as high as aerobic CO2 production potential (10.6 ± 1.5 μmol C g−1 d−1), while CH4 production was low (mean of 7.8 ± 1.5 nmol C g−1 d−1). Denitrification enzyme activity indicated a very high denitrification potential (197 ± 23 μg N g−1 d−1), but net NO 3 − reduction suggested this was a relatively minor pathway for anaerobic CO2 production. Abundances...
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Tags: Monitoring 1-Changes in Plant and Animal Distribution: Ecosystems
Categories: Data,
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Types: Citation,
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Tags: P3b-Vegatation Productivity Changes Due to Temperature change
Categories: Data,
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Tags: Baseline 2-Maps of Anthropogenic Disturbances
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Tags: R2a-Impact Climate Change Vegatation and Subsistence
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Tags: Monitoring 5-Physical Science
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Tags: Relationship Understanding 2b-Effects of Fire on Ecosystems
The boreal forest contains large reserves of carbon. Across this region, wildfires influence the temporal and spatial dynamics of carbon storage. In this study, we estimate fire emissions and changes in carbon storage for boreal North America over the 21st century. We use a gridded data set developed with a multivariate adaptive regression spline approach to determine how area burned varies each year with changing climatic and fuel moisture conditions. We apply the process-based Terrestrial Ecosystem Model to evaluate the role of future fire on the carbon dynamics of boreal North America in the context of changing atmospheric carbon dioxide (CO2) concentration and climate in the A2 and B2 emissions scenarios of...
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Tags: Relationship Understanding 2b-Effects of Fire on Ecosystems
Categories: Data,
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Types: Citation,
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Tags: P2-Changes in Plant and Animal Species Due to Climate Change
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