Climate Cold Regions
20. ABSTRACT ~ BIll,.".,. al6 II ~ "-lderttllT by block number) The Caribou-Poker Creeks Research Watershed is a small (1 01.5-km2) drainage basin located 48 km northwest of Fairbanks, Alaska. Elevations wit!lin the watershed range from 210 to 826 m, and approximately 28 % of its area is u...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.637.3584 2023-05-15T15:53:35+02:00 Climate Cold Regions R. K. Haugen C. W. Slaughter K. E. Howe S. L. Dingman Watershed Alaska The Pennsylvania State University CiteSeerX Archives 1982 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.637.3584 http://www.lter.uaf.edu/pdf/29_Haugen_Slaughter_1982.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.637.3584 http://www.lter.uaf.edu/pdf/29_Haugen_Slaughter_1982.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.lter.uaf.edu/pdf/29_Haugen_Slaughter_1982.pdf SCHEDULE text 1982 ftciteseerx 2016-01-08T15:45:44Z 20. ABSTRACT ~ BIll,.".,. al6 II ~ "-lderttllT by block number) The Caribou-Poker Creeks Research Watershed is a small (1 01.5-km2) drainage basin located 48 km northwest of Fairbanks, Alaska. Elevations wit!lin the watershed range from 210 to 826 m, and approximately 28 % of its area is underlain by permafrost. Climatic differences between the watershed and Fairbanks are primarily due to the higher elevation of the watershed. Generally the watershed climatic sites are warmer in winter and cooler in summer than Text Caribou-Poker Creeks Research Watershed permafrost Alaska Unknown Fairbanks |
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Unknown |
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English |
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SCHEDULE |
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SCHEDULE R. K. Haugen C. W. Slaughter K. E. Howe S. L. Dingman Watershed Alaska Climate Cold Regions |
topic_facet |
SCHEDULE |
description |
20. ABSTRACT ~ BIll,.".,. al6 II ~ "-lderttllT by block number) The Caribou-Poker Creeks Research Watershed is a small (1 01.5-km2) drainage basin located 48 km northwest of Fairbanks, Alaska. Elevations wit!lin the watershed range from 210 to 826 m, and approximately 28 % of its area is underlain by permafrost. Climatic differences between the watershed and Fairbanks are primarily due to the higher elevation of the watershed. Generally the watershed climatic sites are warmer in winter and cooler in summer than |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
R. K. Haugen C. W. Slaughter K. E. Howe S. L. Dingman Watershed Alaska |
author_facet |
R. K. Haugen C. W. Slaughter K. E. Howe S. L. Dingman Watershed Alaska |
author_sort |
R. K. Haugen |
title |
Climate Cold Regions |
title_short |
Climate Cold Regions |
title_full |
Climate Cold Regions |
title_fullStr |
Climate Cold Regions |
title_full_unstemmed |
Climate Cold Regions |
title_sort |
climate cold regions |
publishDate |
1982 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.637.3584 http://www.lter.uaf.edu/pdf/29_Haugen_Slaughter_1982.pdf |
geographic |
Fairbanks |
geographic_facet |
Fairbanks |
genre |
Caribou-Poker Creeks Research Watershed permafrost Alaska |
genre_facet |
Caribou-Poker Creeks Research Watershed permafrost Alaska |
op_source |
http://www.lter.uaf.edu/pdf/29_Haugen_Slaughter_1982.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.637.3584 http://www.lter.uaf.edu/pdf/29_Haugen_Slaughter_1982.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766388697242009600 |