Daily summary of 10 cm soil temperatures in the Arctic LTER moist acidic experimental plots from 1998 to present, Toolik Lake Field Station, Alaska.

Daily summary of 10 cm soil temperatures in the Arctic LTER moist acidic experimental plots for the control (CT), greenhouse (GH), greenhouse plus nitrogen and phosphorus (GHNP) and nitrogen and phosphorus (NP) plots. Soil temperature probes in the tundra soil were problematic with frost heaving cau...

Full description

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/ 2005
Subjects:
Soil temperature
fertilization
arctic tundra
soil warming
Arctic
Northern Foothills
Brooks Range
Dwarf birch
Ice
north slope
permafrost
Tundra
Alaska
Online Access:http://hdl.handle.net/10255/dryad.11743
http://metacat.lternet.edu/knb/metacat/knb-lter-arc.1608.2/xml
id ftdryad:oai:v1.datadryad.org:10255/dryad.11743
record_format openpolar
spelling ftdryad:oai:v1.datadryad.org:10255/dryad.11743 2023-05-15T14:51:59+02:00 Daily summary of 10 cm soil temperatures in the Arctic LTER moist acidic experimental plots from 1998 to present, Toolik Lake Field Station, Alaska. JimLaundre Toolik Lake Field Station (68 38' N, 149 36'W), LTER acidic tussock site on hill south of Toolik Lake, North Slope of Alaska. 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. W E N S -149.75 W -149.0433 E 68.8 N 68.5 S 1998-08-01 to 2005-09-05 2005 text/plain http://hdl.handle.net/10255/dryad.11743 http://metacat.lternet.edu/knb/metacat/knb-lter-arc.1608.2/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.1608.2/xml knb-lter-arc.1608.2 http://hdl.handle.net/10255/dryad.11743 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 Soil temperature fertilization arctic tundra soil warming dataset 2005 ftdryad 2020-01-01T14:26:10Z Daily summary of 10 cm soil temperatures in the Arctic LTER moist acidic experimental plots for the control (CT), greenhouse (GH), greenhouse plus nitrogen and phosphorus (GHNP) and nitrogen and phosphorus (NP) plots. Soil temperature probes in the tundra soil were problematic with frost heaving causing the depth of measurements to change. In order to provide a consistent year to year temperature record notes on changes in depths were used to select the temperature sensor that was within + or – 3 cm of the 10 cm and then averaged daily. 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 Soil temperature
fertilization
arctic tundra
soil warming
spellingShingle Soil temperature
fertilization
arctic tundra
soil warming
Daily summary of 10 cm soil temperatures in the Arctic LTER moist acidic experimental plots from 1998 to present, Toolik Lake Field Station, Alaska.
topic_facet Soil temperature
fertilization
arctic tundra
soil warming
description Daily summary of 10 cm soil temperatures in the Arctic LTER moist acidic experimental plots for the control (CT), greenhouse (GH), greenhouse plus nitrogen and phosphorus (GHNP) and nitrogen and phosphorus (NP) plots. Soil temperature probes in the tundra soil were problematic with frost heaving causing the depth of measurements to change. In order to provide a consistent year to year temperature record notes on changes in depths were used to select the temperature sensor that was within + or – 3 cm of the 10 cm and then averaged daily.
author2 JimLaundre
format Dataset
title Daily summary of 10 cm soil temperatures in the Arctic LTER moist acidic experimental plots from 1998 to present, Toolik Lake Field Station, Alaska.
title_short Daily summary of 10 cm soil temperatures in the Arctic LTER moist acidic experimental plots from 1998 to present, Toolik Lake Field Station, Alaska.
title_full Daily summary of 10 cm soil temperatures in the Arctic LTER moist acidic experimental plots from 1998 to present, Toolik Lake Field Station, Alaska.
title_fullStr Daily summary of 10 cm soil temperatures in the Arctic LTER moist acidic experimental plots from 1998 to present, Toolik Lake Field Station, Alaska.
title_full_unstemmed Daily summary of 10 cm soil temperatures in the Arctic LTER moist acidic experimental plots from 1998 to present, Toolik Lake Field Station, Alaska.
title_sort daily summary of 10 cm soil temperatures in the arctic lter moist acidic experimental plots from 1998 to present, toolik lake field station, alaska.
publisher ARC LTERThe Ecosystems CenterMarine Biological Lab7 MBL StWoods HoleMA02543USA(508) 289 7496arc_im@mbl.eduhttp://ecosystems.mbl.edu/ARC/
publishDate 2005
url http://hdl.handle.net/10255/dryad.11743
http://metacat.lternet.edu/knb/metacat/knb-lter-arc.1608.2/xml
op_coverage Toolik Lake Field Station (68 38' N, 149 36'W), LTER acidic tussock site on hill south of Toolik Lake, North Slope of Alaska.
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.
W E N S
-149.75 W -149.0433 E 68.8 N 68.5 S
1998-08-01 to 2005-09-05
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.1608.2/xml
knb-lter-arc.1608.2
http://hdl.handle.net/10255/dryad.11743
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_ 1766323112141389824

Similar Items