Groundwater Contribution to Winter Streamflows in Alpine Watersheds ...
Alpine watersheds represent an important source of freshwater in western Canada. Since rainfall, snowmelt, and glacier melt make minimal contributions to streamflow during winter months, essentially all winter flow in unregulated streams is provided by groundwater discharge. The analysis of winter f...
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2016
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Online Access: | https://dx.doi.org/10.11575/prism/26327 https://prism.ucalgary.ca/handle/11023/2957 |
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ftdatacite:10.11575/prism/26327 2023-11-05T03:42:08+01:00 Groundwater Contribution to Winter Streamflows in Alpine Watersheds ... Paznekas, Andrius 2016 https://dx.doi.org/10.11575/prism/26327 https://prism.ucalgary.ca/handle/11023/2957 en eng Graduate Studies University of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission. Atmospheric Sciences FOS Earth and related environmental sciences Geology Geophysics Hydrology Alpine Winter streamflow baseflow article master thesis CreativeWork Other 2016 ftdatacite https://doi.org/10.11575/prism/26327 2023-10-09T10:52:07Z Alpine watersheds represent an important source of freshwater in western Canada. Since rainfall, snowmelt, and glacier melt make minimal contributions to streamflow during winter months, essentially all winter flow in unregulated streams is provided by groundwater discharge. The analysis of winter flow in small to medium scale watersheds (21 to 3900 km2) provides critical information regarding the magnitude of groundwater discharge and its relation to the physiographical characteristics of watersheds such as climate, geology, and topography. Furthermore, hydrologic modelling of a small alpine watershed (4.5 km2) provides insight into the storage mechanisms controlling consistent winter flows. Winter flows were in a narrow range (0.2-0.6 mm d-1) throughout the study area, which suggests that the groundwater storage is filled to the maximum capacity every year, and that the groundwater discharge in winter is mostly controlled by the stationary factors such as the spatial variability of geology, topography, and ... Master Thesis glacier* DataCite Metadata Store (German National Library of Science and Technology) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Atmospheric Sciences FOS Earth and related environmental sciences Geology Geophysics Hydrology Alpine Winter streamflow baseflow |
spellingShingle |
Atmospheric Sciences FOS Earth and related environmental sciences Geology Geophysics Hydrology Alpine Winter streamflow baseflow Paznekas, Andrius Groundwater Contribution to Winter Streamflows in Alpine Watersheds ... |
topic_facet |
Atmospheric Sciences FOS Earth and related environmental sciences Geology Geophysics Hydrology Alpine Winter streamflow baseflow |
description |
Alpine watersheds represent an important source of freshwater in western Canada. Since rainfall, snowmelt, and glacier melt make minimal contributions to streamflow during winter months, essentially all winter flow in unregulated streams is provided by groundwater discharge. The analysis of winter flow in small to medium scale watersheds (21 to 3900 km2) provides critical information regarding the magnitude of groundwater discharge and its relation to the physiographical characteristics of watersheds such as climate, geology, and topography. Furthermore, hydrologic modelling of a small alpine watershed (4.5 km2) provides insight into the storage mechanisms controlling consistent winter flows. Winter flows were in a narrow range (0.2-0.6 mm d-1) throughout the study area, which suggests that the groundwater storage is filled to the maximum capacity every year, and that the groundwater discharge in winter is mostly controlled by the stationary factors such as the spatial variability of geology, topography, and ... |
format |
Master Thesis |
author |
Paznekas, Andrius |
author_facet |
Paznekas, Andrius |
author_sort |
Paznekas, Andrius |
title |
Groundwater Contribution to Winter Streamflows in Alpine Watersheds ... |
title_short |
Groundwater Contribution to Winter Streamflows in Alpine Watersheds ... |
title_full |
Groundwater Contribution to Winter Streamflows in Alpine Watersheds ... |
title_fullStr |
Groundwater Contribution to Winter Streamflows in Alpine Watersheds ... |
title_full_unstemmed |
Groundwater Contribution to Winter Streamflows in Alpine Watersheds ... |
title_sort |
groundwater contribution to winter streamflows in alpine watersheds ... |
publisher |
Graduate Studies |
publishDate |
2016 |
url |
https://dx.doi.org/10.11575/prism/26327 https://prism.ucalgary.ca/handle/11023/2957 |
genre |
glacier* |
genre_facet |
glacier* |
op_rights |
University of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission. |
op_doi |
https://doi.org/10.11575/prism/26327 |
_version_ |
1781699048775876608 |