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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Bibliographic Details
Main Author: Paznekas, Andrius
Format: Master Thesis
Language:English
Published: Graduate Studies 2016
Subjects:
Online Access:https://dx.doi.org/10.11575/prism/26327
https://prism.ucalgary.ca/handle/11023/2957
id ftdatacite:10.11575/prism/26327
record_format openpolar
spelling 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
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