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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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) |
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Open Polar |
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Unknown |
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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. |
_version_ |
1766396509806395392 |