This is a Preprint and has not been peer reviewed. This is version 1 of this Preprint.
Downloads
Supplementary Files
Authors
Abstract
The highly-glacierized headwaters of the Kaskawulsh River are home to 9% of all glacier ice in Yukon, Canada, have been losing glacier mass at regionally representative rates, and were the source of a sudden meltwater-rerouting event in 2016 that has had significant downstream consequences. We use an enhanced temperature-index melt model driven by downscaled and bias-corrected climate reanalysis data to estimate the 1980-2022 glacier mass balance, discharge, and water budget of the Kaskawulsh River headwaters. We estimate a catchment-wide cumulative mass loss of 18.02 Gt over 1980-2022 (-0.38 +- 0.15 m w.e./a) and a mean annual discharge of ~60 m3/s, 25% of which originates from non-renewable glacier wastage. The water budget is dominated by glacier ice melt, accounting for 61% of mean annual discharge, followed by snowmelt at 31%, rainfall at 6%, and melt from refrozen ice layers at 2%. Extreme negative and positive mass-balance years produce the largest perturbations in glacier ice melt contributions to the water budget, ranging from a maximum of 67% following negative years to a minimum of 53% in positive years. Catchment-wide discharge increased by 3.90 m3/s per decade from 1980-2022, with statistically significant contributions from glacier ice melt (2.80 m3/s per decade) and rainfall (0.47 m3/s per decade). Rising air temperatures and declining spring snowfall have lead to seasonally accelerated snowline retreat, earlier ice exposure, and earlier onset of net ablation in the catchment at a rate of ~5 days per decade. Based on summer air temperatures projected by CMIP6, and the empirical sensitivities of modelled runoff we calculate for 1980-2022, we hypothesize a more than doubling of annual runoff from this catchment by 2080-2100. This result, combined with a decrease in the variability of discharge from glacier ice melt over 1980-2022, suggests that this catchment is unlikely to
reach "peak water'' (i.e. peak glacier contribution to catchment runoff) this century.
DOI
https://doi.org/10.31223/X5PQ7H
Subjects
Glaciology, Hydrology
Keywords
Glacier runoff, Water budget, Glacierized catchment, Peak water, climate change, St. Elias Mountains
Dates
Published: 2024-11-29 21:53
Last Updated: 2024-11-30 05:53
License
CC BY Attribution 4.0 International
Additional Metadata
Conflict of interest statement:
None
Data Availability (Reason not available):
Daily and annual discharge data from the Dezadeash River, Alsek River above Bates River, and Alsek River near Yakutat hydrometric stations were downloaded from the Environment and Climate Change Canada Historical Hydrometric Data web site https://wateroffice.ec.gc.ca/mainmenu/historical_data_index_e.html. The Kaskawulsh Glacier outline was obtained from https://www.glims.org/maps/glims. The raw NARR data downscaled for this study were obtained from https://downloads.psl.noaa.gov/Datasets/NARR, and the downscaled temperature data for the Kaskawulsh River Headwaters can be found at: https://doi.org/10.5281/zenodo.14010407, and downscaled precipitation data can be found at: https://doi.org/10.5281/zenodo.14014495. Other inputs used to run the mass-balance model can be downloaded at: https://doi.org/10.5281/zenodo.14010158. The model outputs (spanning 1980-2022) used to conduct the analyses presented in this paper can be downloaded at: https://doi.org/10.5281/zenodo.14010257. Downscaling and melt-model code will be made public on github upon manuscript publication.
There are no comments or no comments have been made public for this article.