CONTRIBUTION OF THE DEMING GLACIER TO STREAMFLOW IN THE MIDDLE FORK NOOKSACK

In the North Cascade Range, Washington snowpack accumulation and the resultant ablation provides critical summer water resources. Direct measurement of ablation on the Easton Glacier during 2002 and 2003 allowed determination of glacier runoff from the adjacent Deming Glacier. The summer of 2002 was...

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Other Authors: The Pennsylvania State University CiteSeerX Archives
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Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.178.7135
http://www.nichols.edu/departments/glacier/deming.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.178.7135 2023-05-15T16:00:32+02:00 CONTRIBUTION OF THE DEMING GLACIER TO STREAMFLOW IN THE MIDDLE FORK NOOKSACK The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.178.7135 http://www.nichols.edu/departments/glacier/deming.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.178.7135 http://www.nichols.edu/departments/glacier/deming.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.nichols.edu/departments/glacier/deming.pdf text ftciteseerx 2016-01-07T16:21:17Z In the North Cascade Range, Washington snowpack accumulation and the resultant ablation provides critical summer water resources. Direct measurement of ablation on the Easton Glacier during 2002 and 2003 allowed determination of glacier runoff from the adjacent Deming Glacier. The summer of 2002 was relatively cool and wet and followed a wet winter, as a result the contribution of the Deming Glacier reached a high of 23.9 % of total flow. In 2003 a drier summer followed a dry winter and the maximum glacier contribution was 30.9 % with three months of greater than 20 % contribution Text Deming Glacier Unknown Deming Glacier ENVELOPE(168.500,168.500,-72.000,-72.000)
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description In the North Cascade Range, Washington snowpack accumulation and the resultant ablation provides critical summer water resources. Direct measurement of ablation on the Easton Glacier during 2002 and 2003 allowed determination of glacier runoff from the adjacent Deming Glacier. The summer of 2002 was relatively cool and wet and followed a wet winter, as a result the contribution of the Deming Glacier reached a high of 23.9 % of total flow. In 2003 a drier summer followed a dry winter and the maximum glacier contribution was 30.9 % with three months of greater than 20 % contribution
author2 The Pennsylvania State University CiteSeerX Archives
format Text
title CONTRIBUTION OF THE DEMING GLACIER TO STREAMFLOW IN THE MIDDLE FORK NOOKSACK
spellingShingle CONTRIBUTION OF THE DEMING GLACIER TO STREAMFLOW IN THE MIDDLE FORK NOOKSACK
title_short CONTRIBUTION OF THE DEMING GLACIER TO STREAMFLOW IN THE MIDDLE FORK NOOKSACK
title_full CONTRIBUTION OF THE DEMING GLACIER TO STREAMFLOW IN THE MIDDLE FORK NOOKSACK
title_fullStr CONTRIBUTION OF THE DEMING GLACIER TO STREAMFLOW IN THE MIDDLE FORK NOOKSACK
title_full_unstemmed CONTRIBUTION OF THE DEMING GLACIER TO STREAMFLOW IN THE MIDDLE FORK NOOKSACK
title_sort contribution of the deming glacier to streamflow in the middle fork nooksack
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.178.7135
http://www.nichols.edu/departments/glacier/deming.pdf
long_lat ENVELOPE(168.500,168.500,-72.000,-72.000)
geographic Deming Glacier
geographic_facet Deming Glacier
genre Deming Glacier
genre_facet Deming Glacier
op_source http://www.nichols.edu/departments/glacier/deming.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.178.7135
http://www.nichols.edu/departments/glacier/deming.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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