CO2 flux from tundra lichen, moss, and tussock, Council, Alaska: Assessment of spatial representativeness

CO2 flux-measurement in dominant tundra vegetation on the Seward Peninsula of Alaska was examined for spatial representativeness, using a manual chamber system. In order to assess the representativeness of CO2 flux, a 40 m × 40 m (5-m interval; 81 total points) plot was used in June, August, and Sep...

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Format: Dataset
Language:unknown
Published: International Arctic Research Center (IARC) Data Archive
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Online Access:https://search.dataone.org/view/dcx_62a112d0-876d-41fd-b882-499a62210912_0
id dataone:dcx_62a112d0-876d-41fd-b882-499a62210912_0
record_format openpolar
spelling dataone:dcx_62a112d0-876d-41fd-b882-499a62210912_0 2023-11-08T14:14:57+01:00 CO2 flux from tundra lichen, moss, and tussock, Council, Alaska: Assessment of spatial representativeness ENVELOPE(-168.0,-162.0,67.0,64.0) 2015-05-08T02:02:12.124Z https://search.dataone.org/view/dcx_62a112d0-876d-41fd-b882-499a62210912_0 unknown International Arctic Research Center (IARC) Data Archive tundra lichen moss tussock CO2 flux Seward Peninsula Dataset dataone:urn:node:IARC 2023-11-08T13:37:32Z CO2 flux-measurement in dominant tundra vegetation on the Seward Peninsula of Alaska was examined for spatial representativeness, using a manual chamber system. In order to assess the representativeness of CO2 flux, a 40 m × 40 m (5-m interval; 81 total points) plot was used in June, August, and September of 2011. Average CO2 fluxes in lichen, moss, and tussock tundra were 3.4 ± 2.7, 4.5 ± 2.9, and 7.2 ± 5.7 mgCO2/m2/m during growing season, respectively, suggesting that tussock tundra is a significant CO2 source, especially considering the wide distribution of tussock tundra in the circumpolar region. Further, soil temperature, rather than soil moisture, held the key role in regulating CO2 flux at the study site: CO2 flux from tussock increased linearly as soil temperature increased, while the flux from lichen and moss followed soil temperature nearly exponentially, reflecting differences in surface area covered by the chamber system. Regarding sample size, the 81 total sampling points over June, August, and September satisfy an experimental average that falls within ±10% of full sample average, with a 95% confidence level. However, the number of sampling points for each variety of vegetation during each month must provide at least ±20%, with an 80% confidence level. In order to overcome the logistical constraints, we were required to identify the site’s characteristics with a manual chamber system over a 40 m × 40 m plot and to subsequently employ an automated chamber for spatiotemporal representativeness. Dataset Seward Peninsula Tundra Alaska International Arctic Research Center (IARC) Data Archive (via DataONE) ENVELOPE(-168.0,-162.0,67.0,64.0)
institution Open Polar
collection International Arctic Research Center (IARC) Data Archive (via DataONE)
op_collection_id dataone:urn:node:IARC
language unknown
topic tundra
lichen
moss
tussock
CO2 flux
Seward Peninsula
spellingShingle tundra
lichen
moss
tussock
CO2 flux
Seward Peninsula
CO2 flux from tundra lichen, moss, and tussock, Council, Alaska: Assessment of spatial representativeness
topic_facet tundra
lichen
moss
tussock
CO2 flux
Seward Peninsula
description CO2 flux-measurement in dominant tundra vegetation on the Seward Peninsula of Alaska was examined for spatial representativeness, using a manual chamber system. In order to assess the representativeness of CO2 flux, a 40 m × 40 m (5-m interval; 81 total points) plot was used in June, August, and September of 2011. Average CO2 fluxes in lichen, moss, and tussock tundra were 3.4 ± 2.7, 4.5 ± 2.9, and 7.2 ± 5.7 mgCO2/m2/m during growing season, respectively, suggesting that tussock tundra is a significant CO2 source, especially considering the wide distribution of tussock tundra in the circumpolar region. Further, soil temperature, rather than soil moisture, held the key role in regulating CO2 flux at the study site: CO2 flux from tussock increased linearly as soil temperature increased, while the flux from lichen and moss followed soil temperature nearly exponentially, reflecting differences in surface area covered by the chamber system. Regarding sample size, the 81 total sampling points over June, August, and September satisfy an experimental average that falls within ±10% of full sample average, with a 95% confidence level. However, the number of sampling points for each variety of vegetation during each month must provide at least ±20%, with an 80% confidence level. In order to overcome the logistical constraints, we were required to identify the site’s characteristics with a manual chamber system over a 40 m × 40 m plot and to subsequently employ an automated chamber for spatiotemporal representativeness.
format Dataset
title CO2 flux from tundra lichen, moss, and tussock, Council, Alaska: Assessment of spatial representativeness
title_short CO2 flux from tundra lichen, moss, and tussock, Council, Alaska: Assessment of spatial representativeness
title_full CO2 flux from tundra lichen, moss, and tussock, Council, Alaska: Assessment of spatial representativeness
title_fullStr CO2 flux from tundra lichen, moss, and tussock, Council, Alaska: Assessment of spatial representativeness
title_full_unstemmed CO2 flux from tundra lichen, moss, and tussock, Council, Alaska: Assessment of spatial representativeness
title_sort co2 flux from tundra lichen, moss, and tussock, council, alaska: assessment of spatial representativeness
publisher International Arctic Research Center (IARC) Data Archive
publishDate
url https://search.dataone.org/view/dcx_62a112d0-876d-41fd-b882-499a62210912_0
op_coverage ENVELOPE(-168.0,-162.0,67.0,64.0)
long_lat ENVELOPE(-168.0,-162.0,67.0,64.0)
genre Seward Peninsula
Tundra
Alaska
genre_facet Seward Peninsula
Tundra
Alaska
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