The Effect of Storage on Runoff from a Headwater Subarctic Shield Basin

ABSTRACT. Canadian Shield runoff production processes have been investigated, but research is needed beyond the hillslope scale to determine the influences on the volume and timing of runoff from headwater basins to higher-order streams. Such research will permit an understanding of the magnitude of...

Full description

Bibliographic Details
Main Author: Christopher Spence
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2000
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.497.5490
http://pubs.aina.ucalgary.ca/arctic/Arctic53-3-237.pdf
id ftciteseerx:oai:CiteSeerX.psu:10.1.1.497.5490
record_format openpolar
spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.497.5490 2023-05-15T14:19:51+02:00 The Effect of Storage on Runoff from a Headwater Subarctic Shield Basin Christopher Spence The Pennsylvania State University CiteSeerX Archives 2000 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.497.5490 http://pubs.aina.ucalgary.ca/arctic/Arctic53-3-237.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.497.5490 http://pubs.aina.ucalgary.ca/arctic/Arctic53-3-237.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://pubs.aina.ucalgary.ca/arctic/Arctic53-3-237.pdf text 2000 ftciteseerx 2016-01-08T08:51:37Z ABSTRACT. Canadian Shield runoff production processes have been investigated, but research is needed beyond the hillslope scale to determine the influences on the volume and timing of runoff from headwater basins to higher-order streams. Such research will permit an understanding of the magnitude of climate change impacts at the watershed scale, where changes in the hydrologic regime are felt most by water resource users. To this end, water budget terms were measured over different portions of a headwater lake basin north of Yellowknife, Northwest Territories, during the spring snowmelt of 1998 to determine the relative importance of each component as water moved through the basin. Evaporation made up 16 % and runoff 70 % of the snowmelt from upland areas. Upland ponding of water during the melt increased the evaporative loss. Headwater lake storage deficits are very important in the timing and volume of runoff that is transmitted downstream: 53 % of basin meltwater went to meeting the storage deficit in the lake so that only 7 % of the meltwater was routed out of the basin. These results imply that topology of shield headwater basins, notably the location of lakes and antecedent water levels in lakes, are important in determining the runoff response. As storage deficits in surface waters will cause changes over space in runoff response and timing, it may be inappropriate to consider the snowpack or rainfall volume in isolation when forecasting runoff volume. These results are important for water management and hydrological modeling applications of northern shield basins. Key words: Canadian Shield, Northwest Territories, runoff, snowmelt, water management RÉSUMÉ. On a étudié les processus qui entraînent la production de ruissellement sur le Bouclier canadien, mais il faut envisager Text Arctic Northwest Territories Subarctic Yellowknife Unknown Northwest Territories Yellowknife
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description ABSTRACT. Canadian Shield runoff production processes have been investigated, but research is needed beyond the hillslope scale to determine the influences on the volume and timing of runoff from headwater basins to higher-order streams. Such research will permit an understanding of the magnitude of climate change impacts at the watershed scale, where changes in the hydrologic regime are felt most by water resource users. To this end, water budget terms were measured over different portions of a headwater lake basin north of Yellowknife, Northwest Territories, during the spring snowmelt of 1998 to determine the relative importance of each component as water moved through the basin. Evaporation made up 16 % and runoff 70 % of the snowmelt from upland areas. Upland ponding of water during the melt increased the evaporative loss. Headwater lake storage deficits are very important in the timing and volume of runoff that is transmitted downstream: 53 % of basin meltwater went to meeting the storage deficit in the lake so that only 7 % of the meltwater was routed out of the basin. These results imply that topology of shield headwater basins, notably the location of lakes and antecedent water levels in lakes, are important in determining the runoff response. As storage deficits in surface waters will cause changes over space in runoff response and timing, it may be inappropriate to consider the snowpack or rainfall volume in isolation when forecasting runoff volume. These results are important for water management and hydrological modeling applications of northern shield basins. Key words: Canadian Shield, Northwest Territories, runoff, snowmelt, water management RÉSUMÉ. On a étudié les processus qui entraînent la production de ruissellement sur le Bouclier canadien, mais il faut envisager
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Christopher Spence
spellingShingle Christopher Spence
The Effect of Storage on Runoff from a Headwater Subarctic Shield Basin
author_facet Christopher Spence
author_sort Christopher Spence
title The Effect of Storage on Runoff from a Headwater Subarctic Shield Basin
title_short The Effect of Storage on Runoff from a Headwater Subarctic Shield Basin
title_full The Effect of Storage on Runoff from a Headwater Subarctic Shield Basin
title_fullStr The Effect of Storage on Runoff from a Headwater Subarctic Shield Basin
title_full_unstemmed The Effect of Storage on Runoff from a Headwater Subarctic Shield Basin
title_sort effect of storage on runoff from a headwater subarctic shield basin
publishDate 2000
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.497.5490
http://pubs.aina.ucalgary.ca/arctic/Arctic53-3-237.pdf
geographic Northwest Territories
Yellowknife
geographic_facet Northwest Territories
Yellowknife
genre Arctic
Northwest Territories
Subarctic
Yellowknife
genre_facet Arctic
Northwest Territories
Subarctic
Yellowknife
op_source http://pubs.aina.ucalgary.ca/arctic/Arctic53-3-237.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.497.5490
http://pubs.aina.ucalgary.ca/arctic/Arctic53-3-237.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
_version_ 1766291568240623616