Environmental and vegetation controls on the spatial variability of CH<inf>4</inf> emission from wet-sedge and tussock tundra ecosystems in the Arctic. McEwing, K., Fisher, J., & Zona, D. Plant and Soil, 2015. abstract bibtex © 2015, The Author(s). Aims: Despite multiple studies investigating the environmental controls on CH 4 fluxes from arctic tundra ecosystems, the high spatial variability of CH 4 emissions is not fully understood. This makes the upscaling of CH 4 fluxes from plot to regional scale, particularly challenging. The goal of this study is to refine our knowledge of the spatial variability and controls on CH 4 emission from tundra ecosystems. Methods: CH 4 fluxes were measured in four sites across a variety of wet-sedge and tussock tundra ecosystems in Alaska using chambers and a Los Gatos CO 2 and CH 4 gas analyser. Results: All sites were found to be sources of CH 4 , with northern sites (in Barrow) showing similar CH 4 emission rates to the southernmost site (ca. 300 km south, Ivotuk). Gross primary productivity (GPP), water level and soil temperature were the most important environmental controls on CH 4 emission. Greater vascular plant cover was linked with higher CH 4 emission, but this increased emission with increased vascular plant cover was much higher (86 %) in the drier sites, than the wettest sites (30 %), suggesting that transport and/or substrate availability were crucial limiting factors for CH 4 emission in these tundra ecosystems. Conclusions: Overall, this study provides an increased understanding of the fine scale spatial controls on CH 4 flux, in particular the key role that plant cover and GPP play in enhancing CH 4 emissions from tundra soils.
@article{
title = {Environmental and vegetation controls on the spatial variability of CH<inf>4</inf> emission from wet-sedge and tussock tundra ecosystems in the Arctic},
type = {article},
year = {2015},
identifiers = {[object Object]},
keywords = {Arctic,Climate change,Greenhouse gas emission,Permafrost,Vegetation control},
volume = {388},
id = {8858f1e6-4a0a-3fc3-a88a-538bbd663414},
created = {2018-04-05T23:20:52.441Z},
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last_modified = {2018-04-05T23:20:52.441Z},
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abstract = {© 2015, The Author(s). Aims: Despite multiple studies investigating the environmental controls on CH 4 fluxes from arctic tundra ecosystems, the high spatial variability of CH 4 emissions is not fully understood. This makes the upscaling of CH 4 fluxes from plot to regional scale, particularly challenging. The goal of this study is to refine our knowledge of the spatial variability and controls on CH 4 emission from tundra ecosystems. Methods: CH 4 fluxes were measured in four sites across a variety of wet-sedge and tussock tundra ecosystems in Alaska using chambers and a Los Gatos CO 2 and CH 4 gas analyser. Results: All sites were found to be sources of CH 4 , with northern sites (in Barrow) showing similar CH 4 emission rates to the southernmost site (ca. 300 km south, Ivotuk). Gross primary productivity (GPP), water level and soil temperature were the most important environmental controls on CH 4 emission. Greater vascular plant cover was linked with higher CH 4 emission, but this increased emission with increased vascular plant cover was much higher (86 %) in the drier sites, than the wettest sites (30 %), suggesting that transport and/or substrate availability were crucial limiting factors for CH 4 emission in these tundra ecosystems. Conclusions: Overall, this study provides an increased understanding of the fine scale spatial controls on CH 4 flux, in particular the key role that plant cover and GPP play in enhancing CH 4 emissions from tundra soils.},
bibtype = {article},
author = {McEwing, K.R. and Fisher, J.P. and Zona, D.},
journal = {Plant and Soil},
number = {1-2}
}
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Aims: Despite multiple studies investigating the environmental controls on CH 4 fluxes from arctic tundra ecosystems, the high spatial variability of CH 4 emissions is not fully understood. This makes the upscaling of CH 4 fluxes from plot to regional scale, particularly challenging. The goal of this study is to refine our knowledge of the spatial variability and controls on CH 4 emission from tundra ecosystems. Methods: CH 4 fluxes were measured in four sites across a variety of wet-sedge and tussock tundra ecosystems in Alaska using chambers and a Los Gatos CO 2 and CH 4 gas analyser. Results: All sites were found to be sources of CH 4 , with northern sites (in Barrow) showing similar CH 4 emission rates to the southernmost site (ca. 300 km south, Ivotuk). Gross primary productivity (GPP), water level and soil temperature were the most important environmental controls on CH 4 emission. Greater vascular plant cover was linked with higher CH 4 emission, but this increased emission with increased vascular plant cover was much higher (86 %) in the drier sites, than the wettest sites (30 %), suggesting that transport and/or substrate availability were crucial limiting factors for CH 4 emission in these tundra ecosystems. Conclusions: Overall, this study provides an increased understanding of the fine scale spatial controls on CH 4 flux, in particular the key role that plant cover and GPP play in enhancing CH 4 emissions from tundra soils.","bibtype":"article","author":"McEwing, K.R. and Fisher, J.P. and Zona, D.","journal":"Plant and Soil","number":"1-2","bibtex":"@article{\n title = {Environmental and vegetation controls on the spatial variability of CH<inf>4</inf> emission from wet-sedge and tussock tundra ecosystems in the Arctic},\n type = {article},\n year = {2015},\n identifiers = {[object Object]},\n keywords = {Arctic,Climate change,Greenhouse gas emission,Permafrost,Vegetation control},\n volume = {388},\n id = {8858f1e6-4a0a-3fc3-a88a-538bbd663414},\n created = {2018-04-05T23:20:52.441Z},\n file_attached = {false},\n profile_id = {93cc1067-253c-3a94-87b0-452b9c9fc1b9},\n last_modified = {2018-04-05T23:20:52.441Z},\n read = {false},\n starred = {false},\n authored = {true},\n confirmed = {false},\n hidden = {false},\n private_publication = {false},\n abstract = {© 2015, The Author(s). 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Greater vascular plant cover was linked with higher CH 4 emission, but this increased emission with increased vascular plant cover was much higher (86 %) in the drier sites, than the wettest sites (30 %), suggesting that transport and/or substrate availability were crucial limiting factors for CH 4 emission in these tundra ecosystems. 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