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.
Other Authors: | |
---|---|
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: | |
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 |
_version_ |
1766319456464666624 |