This site requires Cookies enabled in your browser for login.
Updating ...
WaterNet Home
WaterNet
for
pour le
Canada
Menu
WaterNet
Home
GWFO
Home
Catalogue
Master Index
Data
Centre
Collections
X
Defaults
Select All
Websites
X
Global Water Futures Observatories (GWFO) Global Water Futures (GWF) Global Institute for Water Security (GIWS) International Network of Alpine Research Catchment Hydrology
Legacy Research Programs
X
Changing Cold Regions Network (CCRN) Drought Research Initiative (DRI) International Network of Alpine Research Catchment Hydrology (Legacy Site) Improving Processes & Parameterization for Prediction in Cold Regions Hydrology (IP3) The Mackenzie Global Energy and Water Cycle Experiment (GEWEX) Study (MAGS)
Legacy sites
Map
Utilities
X
Account Settings Create a New Record Record List Alias List Editor
Edit Data Centre
Data Types
. . .
X
Clear
Select All
Advanced Search
Go to Top⇡
Related items loading ...
Fetching Chart ...
Publication Additional Information Download
Publication Type
Journal Article
Authorship
Imran, A., Neary, L.K., Falcone, M.D., Wolfe, B.B., Hall, R.I.
Title
Value of long-term isotope monitoring of an index lake for tracking changes in lake water balances across a northern freshwater landscape
Year
2024
Publication Outlet
Journal of Hydrology: Regional Studies
DOI
https://doi.org/10.1016/j.ejrh.2024.101765
Citation
Imran, A., Neary, L.K., Falcone, M.D., Wolfe, B.B., Hall, R.I. (2024) Value of long-term isotope monitoring of an index lake for tracking changes in lake water balances across a northern freshwater landscape, Journal of Hydrology: Regional Studies
Abstract
Study region The Peace-Athabasca Delta, northeastern Alberta, a Ramsar Wetland of International Importance. Study focus To explore the cause of change in water isotope composition at an ‘index lake’ (δSSL; ‘PAD 18’), a terminal basin where inflow equals evaporation, and the consequences for characterizing lake water balance across a region subject to the same atmospheric conditions. For two decades, water isotope composition at PAD 18 provided a relatively constant, reliable estimate of δSSL, but experienced a pronounced shift in 2020–2021 when average flux-weighted ice-free season relative humidity increased by 4.6% from 66.2% (2015–2019) to 70.8% (2020–2021). Using flux-weighted air temperature and relative humidity data from 2020–2021, an independent calculation of δSSL was determined to be equivalent to the average isotope composition of PAD 18 during 2020–2021. New hydrological insights Results reveal re-equilibration of the lake water with the atmosphere following the rise of relative humidity readily provides an explanation for the change in isotope composition of PAD 18. We demonstrate the importance of accurate characterization of δSSL, via the index lake method, for isotope-mass balance calculations using evaporation-to-inflow ratios from measurement of water isotope compositions of 61 lakes across the PAD in July 2021. Findings highlight the value of an index lake and appropriate parameterization of isotope-mass balance models for assessment and ongoing monitoring of water balances of nearby lakes, especially amidst future climatic variability.
Program Affiliations
GWF: Global Water Futures
Project Affiliations
GWF-NWF: Northern Water Futures
Publication Stage
Published
Download Links
https://doi.org/10.1016/j.ejrh.2024.101765
© 2026 - WaterNet Version 2026-07-08
Global Water Futures Observatories
Powered by
G W F Net
T-2024-09-25-K1wLxdJRVlUK2WgU2tZP23cQ Publication 1.0