18O and 2H in streamflow across Canada

Study region Water samples for isotopic analysis were collected during 2013–2019 at 331 gauging stations across Canada in representative watersheds ranging from the Atlantic to the Pacific to the Arctic Oceans. Drainage area coverage of the network included 56 % of Canada’s landmass (9,984,670 km2)...

Full description

Bibliographic Details
Published in:Journal of Hydrology: Regional Studies
Main Authors: Gibson, J. J., Holmes, T., Stadnyk, T. A., Birks, S. J., Eby, P., Pietroniro, A.
Format: Article in Journal/Newspaper
Language:English
Published: Journal of Hydrology: Regional Studies 2020
Subjects:
Online Access:http://hdl.handle.net/1828/12472
https://doi.org/10.1016/j.ejrh.2020.100754
id ftuvicpubl:oai:dspace.library.uvic.ca:1828/12472
record_format openpolar
spelling ftuvicpubl:oai:dspace.library.uvic.ca:1828/12472 2023-05-15T15:11:26+02:00 18O and 2H in streamflow across Canada Gibson, J. J. Holmes, T. Stadnyk, T. A. Birks, S. J. Eby, P. Pietroniro, A. 2020 application/pdf http://hdl.handle.net/1828/12472 https://doi.org/10.1016/j.ejrh.2020.100754 en eng Journal of Hydrology: Regional Studies Gibson, J. J., Holmes, T., Stadnyk, T. A., Birks, S. J., Eby, P., & Pietroniro, A. (2020). 18O and 2H in streamflow across Canada. Journal of Hydrology: Regional Studies, 32, 1-22. https://doi.org/10.1016/j.ejrh.2020.100754. https://doi.org/10.1016/j.ejrh.2020.100754 http://hdl.handle.net/1828/12472 Stable isotopes Streamflow Hydrology Water sources Water balance Evaporation Transpiration Article 2020 ftuvicpubl https://doi.org/10.1016/j.ejrh.2020.100754 2022-05-19T06:11:00Z Study region Water samples for isotopic analysis were collected during 2013–2019 at 331 gauging stations across Canada in representative watersheds ranging from the Atlantic to the Pacific to the Arctic Oceans. Drainage area coverage of the network included 56 % of Canada’s landmass (9,984,670 km2) and was representative of 91 % of Canada’s annual water yield. Study focus Baseline data, including 4603 18O and 2H analyses, are described to assess potential for process studies and predictive model calibration. New hydrological insights for the region While similar patterns are noted between isotopes in streamflow and precipitation across Canada, systematic evaporative enrichment in streamflow occurs in lake- and wetland-rich areas, and systematic depletion occurs in some mountainous and/or cold-regions watersheds. The latter are attributed to uncertainty in precipitation isotope records, glacial melt and/or permafrost thaw. In δ18O-δ2H space, streamflow characteristically plotted on or below the Canadian Meteoric Water Line (CMWL) (δ2H = 8∙δ18O+8.5) along imbricated Regional River Lines (RRL) displaying a range of regression slopes (4.34–9.31) and intercepts (-54 to +24), reflecting regional variations in isotopic composition of input sources, evaporative enrichment, and tributary mixing. We define the Canadian Rivers Line (CRL) based on the linear regression of flow-weighted mean values of station data (δ2H = 7.89∙δ18O+0.45, r2 = 0.962; n = 161). Funding and in-kind support for analytical costs and logistics was provided by Environment and Climate Change Canada via a Grants and Contributions Agreement and by InnoTech Alberta via an Internal Investment Grant. Faculty Reviewed Article in Journal/Newspaper Arctic Climate change permafrost University of Victoria (Canada): UVicDSpace Arctic Canada Pacific Journal of Hydrology: Regional Studies 32 100754
institution Open Polar
collection University of Victoria (Canada): UVicDSpace
op_collection_id ftuvicpubl
language English
topic Stable isotopes
Streamflow
Hydrology
Water sources
Water balance
Evaporation
Transpiration
spellingShingle Stable isotopes
Streamflow
Hydrology
Water sources
Water balance
Evaporation
Transpiration
Gibson, J. J.
Holmes, T.
Stadnyk, T. A.
Birks, S. J.
Eby, P.
Pietroniro, A.
18O and 2H in streamflow across Canada
topic_facet Stable isotopes
Streamflow
Hydrology
Water sources
Water balance
Evaporation
Transpiration
description Study region Water samples for isotopic analysis were collected during 2013–2019 at 331 gauging stations across Canada in representative watersheds ranging from the Atlantic to the Pacific to the Arctic Oceans. Drainage area coverage of the network included 56 % of Canada’s landmass (9,984,670 km2) and was representative of 91 % of Canada’s annual water yield. Study focus Baseline data, including 4603 18O and 2H analyses, are described to assess potential for process studies and predictive model calibration. New hydrological insights for the region While similar patterns are noted between isotopes in streamflow and precipitation across Canada, systematic evaporative enrichment in streamflow occurs in lake- and wetland-rich areas, and systematic depletion occurs in some mountainous and/or cold-regions watersheds. The latter are attributed to uncertainty in precipitation isotope records, glacial melt and/or permafrost thaw. In δ18O-δ2H space, streamflow characteristically plotted on or below the Canadian Meteoric Water Line (CMWL) (δ2H = 8∙δ18O+8.5) along imbricated Regional River Lines (RRL) displaying a range of regression slopes (4.34–9.31) and intercepts (-54 to +24), reflecting regional variations in isotopic composition of input sources, evaporative enrichment, and tributary mixing. We define the Canadian Rivers Line (CRL) based on the linear regression of flow-weighted mean values of station data (δ2H = 7.89∙δ18O+0.45, r2 = 0.962; n = 161). Funding and in-kind support for analytical costs and logistics was provided by Environment and Climate Change Canada via a Grants and Contributions Agreement and by InnoTech Alberta via an Internal Investment Grant. Faculty Reviewed
format Article in Journal/Newspaper
author Gibson, J. J.
Holmes, T.
Stadnyk, T. A.
Birks, S. J.
Eby, P.
Pietroniro, A.
author_facet Gibson, J. J.
Holmes, T.
Stadnyk, T. A.
Birks, S. J.
Eby, P.
Pietroniro, A.
author_sort Gibson, J. J.
title 18O and 2H in streamflow across Canada
title_short 18O and 2H in streamflow across Canada
title_full 18O and 2H in streamflow across Canada
title_fullStr 18O and 2H in streamflow across Canada
title_full_unstemmed 18O and 2H in streamflow across Canada
title_sort 18o and 2h in streamflow across canada
publisher Journal of Hydrology: Regional Studies
publishDate 2020
url http://hdl.handle.net/1828/12472
https://doi.org/10.1016/j.ejrh.2020.100754
geographic Arctic
Canada
Pacific
geographic_facet Arctic
Canada
Pacific
genre Arctic
Climate change
permafrost
genre_facet Arctic
Climate change
permafrost
op_relation Gibson, J. J., Holmes, T., Stadnyk, T. A., Birks, S. J., Eby, P., & Pietroniro, A. (2020). 18O and 2H in streamflow across Canada. Journal of Hydrology: Regional Studies, 32, 1-22. https://doi.org/10.1016/j.ejrh.2020.100754.
https://doi.org/10.1016/j.ejrh.2020.100754
http://hdl.handle.net/1828/12472
op_doi https://doi.org/10.1016/j.ejrh.2020.100754
container_title Journal of Hydrology: Regional Studies
container_volume 32
container_start_page 100754
_version_ 1766342279301169152