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.
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ARC LTERThe Ecosystems CenterMarine Biological Lab7 MBL StWoods HoleMA02543USA(508) 289 7496arc_im@mbl.eduhttp://ecosystems.mbl.edu/ARC/
2004
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Online Access: | http://hdl.handle.net/10255/dryad.11041 http://metacat.lternet.edu/knb/metacat/knb-lter-arc.1501.4/xml |
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ftdryad:oai:v1.datadryad.org:10255/dryad.11041 |
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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 |