AmeriFlux AmeriFlux CA-SCC Scotty Creek Landscape ...
This is the AmeriFlux version of the carbon flux data for the site CA-SCC Scotty Creek Landscape. Site Description - The Scotty Creek flux tower is located in an organic-rich boreal forest-wetland landscape about 50 km south of Fort Simpson in the Taiga Plains of the Mackenzie watershed. The tower w...
Main Authors: | , |
---|---|
Format: | Dataset |
Language: | English |
Published: |
AmeriFlux; Université de Montréal; Wilfrid Laurier University
2018
|
Subjects: | |
Online Access: | https://dx.doi.org/10.17190/amf/1480303 https://www.osti.gov/servlets/purl/1480303/ |
id |
ftdatacite:10.17190/amf/1480303 |
---|---|
record_format |
openpolar |
spelling |
ftdatacite:10.17190/amf/1480303 2023-12-31T10:06:59+01:00 AmeriFlux AmeriFlux CA-SCC Scotty Creek Landscape ... Sonnentag, Oliver Quinton, William 2018 https://dx.doi.org/10.17190/amf/1480303 https://www.osti.gov/servlets/purl/1480303/ en eng AmeriFlux; Université de Montréal; Wilfrid Laurier University https://dx.doi.org/10.18140/flx/1669628 dataset Dataset Specialized Mix 2018 ftdatacite https://doi.org/10.17190/amf/148030310.18140/flx/1669628 2023-12-01T12:19:50Z This is the AmeriFlux version of the carbon flux data for the site CA-SCC Scotty Creek Landscape. Site Description - The Scotty Creek flux tower is located in an organic-rich boreal forest-wetland landscape about 50 km south of Fort Simpson in the Taiga Plains of the Mackenzie watershed. The tower was installed in 2013 and operates an open-path EC system year-round running on solar power only. Flux footprints contain about 50 % forested peat plateaus and 50 % wetlands (i.e., collapse-scar bogs). The forests are underlain by permafrost, while the treeless wetlands are permafrost-free. The tower itself is located on a forested peat plateau. Black spruce tree density on plateaus is sparse and the mean canopy height is ca. 5 m. ... Dataset Fort Simpson Mackenzie watershed Peat Peat plateau permafrost taiga Taiga plains DataCite Metadata Store (German National Library of Science and Technology) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
description |
This is the AmeriFlux version of the carbon flux data for the site CA-SCC Scotty Creek Landscape. Site Description - The Scotty Creek flux tower is located in an organic-rich boreal forest-wetland landscape about 50 km south of Fort Simpson in the Taiga Plains of the Mackenzie watershed. The tower was installed in 2013 and operates an open-path EC system year-round running on solar power only. Flux footprints contain about 50 % forested peat plateaus and 50 % wetlands (i.e., collapse-scar bogs). The forests are underlain by permafrost, while the treeless wetlands are permafrost-free. The tower itself is located on a forested peat plateau. Black spruce tree density on plateaus is sparse and the mean canopy height is ca. 5 m. ... |
format |
Dataset |
author |
Sonnentag, Oliver Quinton, William |
spellingShingle |
Sonnentag, Oliver Quinton, William AmeriFlux AmeriFlux CA-SCC Scotty Creek Landscape ... |
author_facet |
Sonnentag, Oliver Quinton, William |
author_sort |
Sonnentag, Oliver |
title |
AmeriFlux AmeriFlux CA-SCC Scotty Creek Landscape ... |
title_short |
AmeriFlux AmeriFlux CA-SCC Scotty Creek Landscape ... |
title_full |
AmeriFlux AmeriFlux CA-SCC Scotty Creek Landscape ... |
title_fullStr |
AmeriFlux AmeriFlux CA-SCC Scotty Creek Landscape ... |
title_full_unstemmed |
AmeriFlux AmeriFlux CA-SCC Scotty Creek Landscape ... |
title_sort |
ameriflux ameriflux ca-scc scotty creek landscape ... |
publisher |
AmeriFlux; Université de Montréal; Wilfrid Laurier University |
publishDate |
2018 |
url |
https://dx.doi.org/10.17190/amf/1480303 https://www.osti.gov/servlets/purl/1480303/ |
genre |
Fort Simpson Mackenzie watershed Peat Peat plateau permafrost taiga Taiga plains |
genre_facet |
Fort Simpson Mackenzie watershed Peat Peat plateau permafrost taiga Taiga plains |
op_relation |
https://dx.doi.org/10.18140/flx/1669628 |
op_doi |
https://doi.org/10.17190/amf/148030310.18140/flx/1669628 |
_version_ |
1786839191065198592 |