Montane seasonal and elevational precipitation gradients in the southern Rockies of Alberta, Canada

dc.contributor.authorBarnes, Celeste
dc.contributor.authorMacDonald, Ryan J.
dc.contributor.authorHopkinson, Chris
dc.date.accessioned2025-05-12T22:46:07Z
dc.date.available2025-05-12T22:46:07Z
dc.date.issued2025
dc.descriptionOpen access article. Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International license (CC BY-NC-NC 4.0) applies
dc.description.abstractModelling precipitation inputs in mountainous terrain is challenging for water resource managers given sparse monitoring sites and complex physical hydroclimatic processes. Government of Alberta weather station uncorrected and bias-corrected precipitation datasets were used to examine elevational precipitation gradients (EPGs) and seasonality of EPGs for six South-Saskatchewan River headwater sites (alpine, sub-alpine, valley). January EPG from valley to alpine sites (730 m elevation difference) using uncorrected precipitation was 19 mm/100 m. Corrected EPG was approximately three times greater (61 mm/100 m). The valley received more precipitation than the alpine (inverse EPG) in late spring and summer. A seasonal signal was present whereby all sites demonstrated 50%–70% lower summertime precipitation relative to winter months, with the greatest seasonal variance at the alpine site. Winter watershed-level spatialized precipitation volume was compared to modelled snow water equivalent (SWE) associated with two late-winter airborne lidar surveys. Uncorrected volumes (2020: 64.0 × 106m3, 2021: 63.2 × 106m3) were slightly higher than modelled mean SWE (2020: 51.6 × 106m3, 2021: 44.2 × 106m3) whereas bias-corrected (2020: 120.5 × 106m3, 2021: 119.7 × 106m3) almost doubled the estimate. Corrected precipitation is assumed closer to the true value. Cumulative sublimation, evaporation and snowmelt losses result in ground-level snowpack yield that deviates from total atmospheric precipitation in an increasingly negative manner. The 2020/2021 simulations suggest wintertime atmospheric precipitation exceeds late-winter snowpack accumulation by up to 57% and 63%, respectively. A loss of 16 × 106m3 (7%) watershed SWE from the alpine zone was partially attributed to redistribution downslope to the treeline-ecotone. Physical snowpack losses from sublimation and melt, or modelling uncertainty due to precipitation correction and alpine snow-density uncertainties can also contribute to observed discrepancies between in situ SWE and cumulative precipitation. Ignoring bias-correction in headwater precipitation estimates can greatly impact headwater precipitation volume estimates and ignoring EPG seasonality is likely to result in under-estimated winter and over-estimated summer yields.
dc.description.peer-reviewYes
dc.identifier.citationBarnes, C., MacDonald, R. J., & Hopkinson, C. (2025). Montane seasonal and elevational precipitation gradients in the southern Rockies of Alberta, Canada. Hydrological Processes, 39(1). https://doi.org/10.1002/hyp.70061
dc.identifier.urihttps://hdl.handle.net/10133/7029
dc.language.isoen
dc.publisherWiley
dc.publisher.departmentDepartment of Geography and Environment
dc.publisher.facultyArts and Science
dc.publisher.institutionUniversity of Lethbridge
dc.publisher.institutionMacDonald Hydrology Consultants Ltd.
dc.publisher.urlhttps://doi.org/10.1002/hyp.70061
dc.subjectCanadian Rocky Mountain eastern slopes
dc.subjectElevational precipitation gradients
dc.subjectMountain precipitation
dc.subjectSeasonality
dc.subjectSWE
dc.subjectWater resource management
dc.subject.lcshHydrologic models--Alberta
dc.subject.lcshWater supply--Alberta
dc.subject.lcshWater-supply--Management--Alberta
dc.titleMontane seasonal and elevational precipitation gradients in the southern Rockies of Alberta, Canada
dc.typeArticle
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