Soil temperatures, lake temperature, lake depth, and evaporation pan depth and pan water temperature data from Toolik Field Station, Toolik Lake, Alaska for 2003.

Weather data file for Arctic Tundra LTER site at Toolik Lake. Only the sensors that are measured every 10 minutes and averaged every three hours are include, i.e. soil temperatures, lake temperature, lake depth, and evaporation pan depth and pan water temperature.

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/ 2004
Subjects:
soil temperature
lake temperature
lake depth
evaporation pan
weather
Arctic
Fairbanks
Northern Foothills
Brooks Range
Dwarf birch
Ice
north slope
permafrost
Tundra
Alaska
Online Access:http://hdl.handle.net/10255/dryad.11041
http://metacat.lternet.edu/knb/metacat/knb-lter-arc.1501.4/xml
id ftdryad:oai:v1.datadryad.org:10255/dryad.11041
record_format openpolar
spelling ftdryad:oai:v1.datadryad.org:10255/dryad.11041 2023-05-15T14:59:20+02:00 Soil temperatures, lake temperature, lake depth, and evaporation pan depth and pan water temperature data from Toolik Field Station, Toolik Lake, Alaska for 2003. JIMLAUNDRE University of Alaska Fairbanks Toolik Field Station, North Slope of Alaska Coords in WGS84(ITRF00 - Ep. 1997.0) Accuracy should be good to ~ 90cm 68.628228973N, 149.596001285W, Height (above ellipsoid) is 726.5m, give or take ~1.5m 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. -149.596 W -149.596 E 68.6283 N 68.6283 S -149.75 W -149.0433 E 68.8 N 68.5 S 2003-01-01 to 2003-12-31 2004 text/plain http://hdl.handle.net/10255/dryad.11041 http://metacat.lternet.edu/knb/metacat/knb-lter-arc.1501.4/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.1501.4/xml knb-lter-arc.1501.4 http://hdl.handle.net/10255/dryad.11041 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 lake temperature lake depth evaporation pan weather dataset 2004 ftdryad 2020-01-01T14:24:37Z Weather data file for Arctic Tundra LTER site at Toolik Lake. Only the sensors that are measured every 10 minutes and averaged every three hours are include, i.e. soil temperatures, lake temperature, lake depth, and evaporation pan depth and pan water temperature. Dataset Arctic Brooks Range Dwarf birch Ice north slope permafrost Tundra Alaska Dryad Digital Repository (Duke University) Arctic Fairbanks 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
lake temperature
lake depth
evaporation pan
weather
spellingShingle soil temperature
lake temperature
lake depth
evaporation pan
weather
Soil temperatures, lake temperature, lake depth, and evaporation pan depth and pan water temperature data from Toolik Field Station, Toolik Lake, Alaska for 2003.
topic_facet soil temperature
lake temperature
lake depth
evaporation pan
weather
description Weather data file for Arctic Tundra LTER site at Toolik Lake. Only the sensors that are measured every 10 minutes and averaged every three hours are include, i.e. soil temperatures, lake temperature, lake depth, and evaporation pan depth and pan water temperature.
author2 JIMLAUNDRE
format Dataset
title Soil temperatures, lake temperature, lake depth, and evaporation pan depth and pan water temperature data from Toolik Field Station, Toolik Lake, Alaska for 2003.
title_short Soil temperatures, lake temperature, lake depth, and evaporation pan depth and pan water temperature data from Toolik Field Station, Toolik Lake, Alaska for 2003.
title_full Soil temperatures, lake temperature, lake depth, and evaporation pan depth and pan water temperature data from Toolik Field Station, Toolik Lake, Alaska for 2003.
title_fullStr Soil temperatures, lake temperature, lake depth, and evaporation pan depth and pan water temperature data from Toolik Field Station, Toolik Lake, Alaska for 2003.
title_full_unstemmed Soil temperatures, lake temperature, lake depth, and evaporation pan depth and pan water temperature data from Toolik Field Station, Toolik Lake, Alaska for 2003.
title_sort soil temperatures, lake temperature, lake depth, and evaporation pan depth and pan water temperature data from toolik field station, toolik lake, alaska for 2003.
publisher ARC LTERThe Ecosystems CenterMarine Biological Lab7 MBL StWoods HoleMA02543USA(508) 289 7496arc_im@mbl.eduhttp://ecosystems.mbl.edu/ARC/
publishDate 2004
url http://hdl.handle.net/10255/dryad.11041
http://metacat.lternet.edu/knb/metacat/knb-lter-arc.1501.4/xml
op_coverage University of Alaska Fairbanks Toolik Field Station, North Slope of Alaska Coords in WGS84(ITRF00 - Ep. 1997.0) Accuracy should be good to ~ 90cm 68.628228973N, 149.596001285W, Height (above ellipsoid) is 726.5m, give or take ~1.5m
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.
-149.596 W -149.596 E 68.6283 N 68.6283 S
-149.75 W -149.0433 E 68.8 N 68.5 S
2003-01-01 to 2003-12-31
long_lat ENVELOPE(163.917,163.917,-74.733,-74.733)
geographic Arctic
Fairbanks
Northern Foothills
geographic_facet Arctic
Fairbanks
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.1501.4/xml
knb-lter-arc.1501.4
http://hdl.handle.net/10255/dryad.11041
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_ 1766331444941029376

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