Hydrology of the North Klondike River: carbon export, water balance and inter-annual climate influences within a sub-alpine permafrost catchment

Arctic and sub-arctic watersheds are undergoing significant changes due to recent climate warming and degrading permafrost, engendering enhanced monitoring of arctic rivers. Smaller catchments provide understanding of discharge, solute flux and groundwater recharge at the process level that contribu...

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Published in:Isotopes in Environmental and Health Studies
Main Authors: Lapp, A. (Anthony), Clark, I. (Ian), Macumber, A. (Andrew), Patterson, T. (Tim)
Format: Article in Journal/Newspaper
Language:English
Published: 2017
Subjects:
Online Access:https://ir.library.carleton.ca/pub/14463
https://doi.org/10.1080/10256016.2017.1355795
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record_format openpolar
spelling ftcarletonunivir:oai:carleton.ca:14463 2023-05-15T14:50:22+02:00 Hydrology of the North Klondike River: carbon export, water balance and inter-annual climate influences within a sub-alpine permafrost catchment Lapp, A. (Anthony) Clark, I. (Ian) Macumber, A. (Andrew) Patterson, T. (Tim) 2017-09-03 https://ir.library.carleton.ca/pub/14463 https://doi.org/10.1080/10256016.2017.1355795 en eng https://ir.library.carleton.ca/pub/14463 doi:10.1080/10256016.2017.1355795 Isotopes in Environmental and Health Studies, pp. 1-18 Carbon-13 carbon-14 catchment groundwater hydrogen-2 hydrogen-3 isotope hydrology North Klondike River oxygen-18 sub-alpine permafrost water balance info:eu-repo/semantics/article 2017 ftcarletonunivir https://doi.org/10.1080/10256016.2017.1355795 2022-02-06T21:51:28Z Arctic and sub-arctic watersheds are undergoing significant changes due to recent climate warming and degrading permafrost, engendering enhanced monitoring of arctic rivers. Smaller catchments provide understanding of discharge, solute flux and groundwater recharge at the process level that contributes to an understanding of how larger arctic watersheds are responding to climate change. The North Klondike River, located in west central Yukon, is a sub-alpine permafrost catchment, which maintains an active hydrological monitoring station with a record of >40 years. In addition to being able to monitor intra-annual variability, this data set allows for more complex analysis of streamflow records. Streamflow data, geochemistry and stable isotope data for 2014 show a groundwater-dominated system, predominantly recharged during periods of snowmelt. Radiocarbon is shown to be a valuable tracer of soil zone recharge processes and carbon sources. Winter groundwater baseflow contributes 20 % of total annual discharge, and accounts for up to 50 % of total river discharge during the spring and summer months. Although total stream discharge remains unchanged, mean annual groundwater baseflow has increased over the 40-year monitoring period. Wavelet analysis reveals a catchment that responds to El Niño and longer solar cycles, as well as climatic shifts such as the Pacific Decadal Oscillation. Dedicated to Professor Peter Fritz on the occasion of his 80th birthday. Article in Journal/Newspaper Arctic Climate change permafrost Yukon Carleton University's Institutional Repository Arctic Yukon Pacific Klondike River ENVELOPE(-139.442,-139.442,64.054,64.054) North Klondike River ENVELOPE(-138.692,-138.692,63.962,63.962) Isotopes in Environmental and Health Studies 53 5 500 517
institution Open Polar
collection Carleton University's Institutional Repository
op_collection_id ftcarletonunivir
language English
topic Carbon-13
carbon-14
catchment
groundwater
hydrogen-2
hydrogen-3
isotope hydrology
North Klondike River
oxygen-18
sub-alpine permafrost
water balance
spellingShingle Carbon-13
carbon-14
catchment
groundwater
hydrogen-2
hydrogen-3
isotope hydrology
North Klondike River
oxygen-18
sub-alpine permafrost
water balance
Lapp, A. (Anthony)
Clark, I. (Ian)
Macumber, A. (Andrew)
Patterson, T. (Tim)
Hydrology of the North Klondike River: carbon export, water balance and inter-annual climate influences within a sub-alpine permafrost catchment
topic_facet Carbon-13
carbon-14
catchment
groundwater
hydrogen-2
hydrogen-3
isotope hydrology
North Klondike River
oxygen-18
sub-alpine permafrost
water balance
description Arctic and sub-arctic watersheds are undergoing significant changes due to recent climate warming and degrading permafrost, engendering enhanced monitoring of arctic rivers. Smaller catchments provide understanding of discharge, solute flux and groundwater recharge at the process level that contributes to an understanding of how larger arctic watersheds are responding to climate change. The North Klondike River, located in west central Yukon, is a sub-alpine permafrost catchment, which maintains an active hydrological monitoring station with a record of >40 years. In addition to being able to monitor intra-annual variability, this data set allows for more complex analysis of streamflow records. Streamflow data, geochemistry and stable isotope data for 2014 show a groundwater-dominated system, predominantly recharged during periods of snowmelt. Radiocarbon is shown to be a valuable tracer of soil zone recharge processes and carbon sources. Winter groundwater baseflow contributes 20 % of total annual discharge, and accounts for up to 50 % of total river discharge during the spring and summer months. Although total stream discharge remains unchanged, mean annual groundwater baseflow has increased over the 40-year monitoring period. Wavelet analysis reveals a catchment that responds to El Niño and longer solar cycles, as well as climatic shifts such as the Pacific Decadal Oscillation. Dedicated to Professor Peter Fritz on the occasion of his 80th birthday.
format Article in Journal/Newspaper
author Lapp, A. (Anthony)
Clark, I. (Ian)
Macumber, A. (Andrew)
Patterson, T. (Tim)
author_facet Lapp, A. (Anthony)
Clark, I. (Ian)
Macumber, A. (Andrew)
Patterson, T. (Tim)
author_sort Lapp, A. (Anthony)
title Hydrology of the North Klondike River: carbon export, water balance and inter-annual climate influences within a sub-alpine permafrost catchment
title_short Hydrology of the North Klondike River: carbon export, water balance and inter-annual climate influences within a sub-alpine permafrost catchment
title_full Hydrology of the North Klondike River: carbon export, water balance and inter-annual climate influences within a sub-alpine permafrost catchment
title_fullStr Hydrology of the North Klondike River: carbon export, water balance and inter-annual climate influences within a sub-alpine permafrost catchment
title_full_unstemmed Hydrology of the North Klondike River: carbon export, water balance and inter-annual climate influences within a sub-alpine permafrost catchment
title_sort hydrology of the north klondike river: carbon export, water balance and inter-annual climate influences within a sub-alpine permafrost catchment
publishDate 2017
url https://ir.library.carleton.ca/pub/14463
https://doi.org/10.1080/10256016.2017.1355795
long_lat ENVELOPE(-139.442,-139.442,64.054,64.054)
ENVELOPE(-138.692,-138.692,63.962,63.962)
geographic Arctic
Yukon
Pacific
Klondike River
North Klondike River
geographic_facet Arctic
Yukon
Pacific
Klondike River
North Klondike River
genre Arctic
Climate change
permafrost
Yukon
genre_facet Arctic
Climate change
permafrost
Yukon
op_source Isotopes in Environmental and Health Studies, pp. 1-18
op_relation https://ir.library.carleton.ca/pub/14463
doi:10.1080/10256016.2017.1355795
op_doi https://doi.org/10.1080/10256016.2017.1355795
container_title Isotopes in Environmental and Health Studies
container_volume 53
container_issue 5
container_start_page 500
op_container_end_page 517
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