Late season thaw depth measured in the ARC LTER moist acidic tussock experimental plots at Toolik Field station, AK Arctci LTER 1993 to current year.

Late season thaw depth was measured in the ARC LTER experimental plots (Moist Acidic Tussock, Moist Non-acidicTussock, Moist Non-acidic Non-tussock, Wet Sedge) at Toolik Lake, AK using a thaw probe.

Bibliographic Details
Other Authors: JimLaundre
Format: Dataset
Language:unknown
Published: ARC LTERThe Ecosystems CenterMarine Biological Lab7 MBL StWoods HoleMA02543USA(508) 289 7496arc_im@mbl.eduhttp://ecosystems.mbl.edu/ARC/ 2006
Subjects:
Ice
Online Access:http://hdl.handle.net/10255/dryad.11756
http://metacat.lternet.edu/knb/metacat/knb-lter-arc.1610.4/xml
id ftdryad:oai:v1.datadryad.org:10255/dryad.11756
record_format openpolar
spelling ftdryad:oai:v1.datadryad.org:10255/dryad.11756 2023-05-15T14:48:22+02:00 Late season thaw depth measured in the ARC LTER moist acidic tussock experimental plots at Toolik Field station, AK Arctci LTER 1993 to current year. JimLaundre Arctic LTER, Toolik Field Station, North Slope Alaska(68 degrees 38'N, 149 degrees 34'W, elevation 760 m). Wet Sedge Tundra. Arctic LTER, Toolik Field Station, North Slope Alaska(68 degrees 38'N, 149 degrees 34'W, elevation 760 m). Moist Acidic Tussock Tundra. Arctic LTER, Toolik Field Station, North Slope Alaska(68 degrees 38'N, 149 degrees 34'W, elevation 760 m). Moist Non-acidic Tussock Tundra. The Arctic LTER research site (68°N and 149°W) is in the foothills region of the North Slope of Alaska and includes the entire Toolik Lake watershed and the adjacent watershed of the upper Kuparuk River, down to the confluence of these two watersheds. This area is typical of the northern foothills of the Brooks Range, with continuous permafrost, no trees, a complete snow cover for 7 to 9 months, winter ice cover on lakes, streams, and ocean, and cessation of river flow during the winter. Tussock tundra vegetation of sedges and grasses mixed with dwarf birch and low willows form the dominant vegetation type with areas of drier heath tundra on ridge tops and other well-drained sites as well as areas of river-bottom willow communities. -149.6024 W -149.6024 E 68.6253 N 68.6253 S -149.61058 W -149.61058 E 68.62405 N 68.62405 S -149.64074 W -149.64074 E 68.6342 N 68.6342 S -149.75 W -149.0433 E 68.8 N 68.5 S 1993-08-20 to 2009-08-21 2006 text/plain http://hdl.handle.net/10255/dryad.11756 http://metacat.lternet.edu/knb/metacat/knb-lter-arc.1610.4/xml unknown ARC LTERThe Ecosystems CenterMarine Biological Lab7 MBL StWoods HoleMA02543USA(508) 289 7496arc_im@mbl.eduhttp://ecosystems.mbl.edu/ARC/ http://metacat.lternet.edu/knb/metacat/knb-lter-arc.1610.4/xml knb-lter-arc.1610.4 http://hdl.handle.net/10255/dryad.11756 Acceptance and utilization of LTER data requires that:The Principal Investigator be sent a notice stating reasons for acquiring any data and a description of the publication intentions.The Principal Investigator of the data set be sent a copy of the report or manuscript prior to submission and be adequately cited in any resultant publicationsA copy of any resultant publications should be sent to: Principal Investigator Ecosystems Center Marine Biological Laboratory Woods Hole, MA 02543 arctic tundra thaw depth soil warming soil fertilization disturbance dataset 2006 ftdryad 2020-01-01T14:26:27Z Late season thaw depth was measured in the ARC LTER experimental plots (Moist Acidic Tussock, Moist Non-acidicTussock, Moist Non-acidic Non-tussock, Wet Sedge) at Toolik Lake, AK using a thaw probe. Dataset Arctic Brooks Range Dwarf birch Ice north slope permafrost Tundra Alaska Dryad Digital Repository (Duke University) Arctic Northern Foothills ENVELOPE(163.917,163.917,-74.733,-74.733)
institution Open Polar
collection Dryad Digital Repository (Duke University)
op_collection_id ftdryad
language unknown
topic arctic tundra
thaw depth
soil warming
soil fertilization
disturbance
spellingShingle arctic tundra
thaw depth
soil warming
soil fertilization
disturbance
Late season thaw depth measured in the ARC LTER moist acidic tussock experimental plots at Toolik Field station, AK Arctci LTER 1993 to current year.
topic_facet arctic tundra
thaw depth
soil warming
soil fertilization
disturbance
description Late season thaw depth was measured in the ARC LTER experimental plots (Moist Acidic Tussock, Moist Non-acidicTussock, Moist Non-acidic Non-tussock, Wet Sedge) at Toolik Lake, AK using a thaw probe.
author2 JimLaundre
format Dataset
title Late season thaw depth measured in the ARC LTER moist acidic tussock experimental plots at Toolik Field station, AK Arctci LTER 1993 to current year.
title_short Late season thaw depth measured in the ARC LTER moist acidic tussock experimental plots at Toolik Field station, AK Arctci LTER 1993 to current year.
title_full Late season thaw depth measured in the ARC LTER moist acidic tussock experimental plots at Toolik Field station, AK Arctci LTER 1993 to current year.
title_fullStr Late season thaw depth measured in the ARC LTER moist acidic tussock experimental plots at Toolik Field station, AK Arctci LTER 1993 to current year.
title_full_unstemmed Late season thaw depth measured in the ARC LTER moist acidic tussock experimental plots at Toolik Field station, AK Arctci LTER 1993 to current year.
title_sort late season thaw depth measured in the arc lter moist acidic tussock experimental plots at toolik field station, ak arctci lter 1993 to current year.
publisher ARC LTERThe Ecosystems CenterMarine Biological Lab7 MBL StWoods HoleMA02543USA(508) 289 7496arc_im@mbl.eduhttp://ecosystems.mbl.edu/ARC/
publishDate 2006
url http://hdl.handle.net/10255/dryad.11756
http://metacat.lternet.edu/knb/metacat/knb-lter-arc.1610.4/xml
op_coverage Arctic LTER, Toolik Field Station, North Slope Alaska(68 degrees 38'N, 149 degrees 34'W, elevation 760 m). Wet Sedge Tundra.
Arctic LTER, Toolik Field Station, North Slope Alaska(68 degrees 38'N, 149 degrees 34'W, elevation 760 m). Moist Acidic Tussock Tundra.
Arctic LTER, Toolik Field Station, North Slope Alaska(68 degrees 38'N, 149 degrees 34'W, elevation 760 m). Moist Non-acidic Tussock Tundra.
The Arctic LTER research site (68°N and 149°W) is in the foothills region of the North Slope of Alaska and includes the entire Toolik Lake watershed and the adjacent watershed of the upper Kuparuk River, down to the confluence of these two watersheds. This area is typical of the northern foothills of the Brooks Range, with continuous permafrost, no trees, a complete snow cover for 7 to 9 months, winter ice cover on lakes, streams, and ocean, and cessation of river flow during the winter. Tussock tundra vegetation of sedges and grasses mixed with dwarf birch and low willows form the dominant vegetation type with areas of drier heath tundra on ridge tops and other well-drained sites as well as areas of river-bottom willow communities.
-149.6024 W -149.6024 E 68.6253 N 68.6253 S
-149.61058 W -149.61058 E 68.62405 N 68.62405 S
-149.64074 W -149.64074 E 68.6342 N 68.6342 S
-149.75 W -149.0433 E 68.8 N 68.5 S
1993-08-20 to 2009-08-21
long_lat ENVELOPE(163.917,163.917,-74.733,-74.733)
geographic Arctic
Northern Foothills
geographic_facet Arctic
Northern Foothills
genre Arctic
Brooks Range
Dwarf birch
Ice
north slope
permafrost
Tundra
Alaska
genre_facet Arctic
Brooks Range
Dwarf birch
Ice
north slope
permafrost
Tundra
Alaska
op_relation http://metacat.lternet.edu/knb/metacat/knb-lter-arc.1610.4/xml
knb-lter-arc.1610.4
http://hdl.handle.net/10255/dryad.11756
op_rights Acceptance and utilization of LTER data requires that:The Principal Investigator be sent a notice stating reasons for acquiring any data and a description of the publication intentions.The Principal Investigator of the data set be sent a copy of the report or manuscript prior to submission and be adequately cited in any resultant publicationsA copy of any resultant publications should be sent to: Principal Investigator Ecosystems Center Marine Biological Laboratory Woods Hole, MA 02543
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