Spatially distributed tracer-aided runoff modelling and dynamics of storage and water ages in a permafrost-influenced catchment

Thea I. Piovano, Doerthe Tetzlaff (Corresponding Author), Sean K. Carey, Nadine J. Shatilla, Aaron Smith, Christopher Soulsby

Research output: Contribution to journalArticle

Abstract

Permafrost strongly controls hydrological processes in cold regions. Our understanding of how changes in seasonal and perennial frozen ground disposition and linked storage dynamics affect runoff generation processes remains limited. Storage dynamics and water redistribution are influenced by the seasonal variability and spatial heterogeneity of frozen ground, snow accumulation and melt. Stable isotopes are potentially useful for quantifying the dynamics of water sources, flow paths and ages, yet few studies have employed isotope data in permafrost-influenced catchments. Here, we applied the conceptual model STARR (the Spatially distributed Tracer-Aided Rainfall–Runoff model), which facilitates fully distributed simulations of hydrological storage dynamics and runoff processes, isotopic composition and water ages. We adapted this model for a subarctic catchment in Yukon Territory, Canada, with a time-variable implementation of field capacity to include the influence of thaw dynamics. A multi-criteria calibration based on stream flow, snow water equivalent and isotopes was applied to 3 years of data. The integration of isotope data in the spatially distributed model provided the basis for quantifying spatio-temporal dynamics of water storage and ages, emphasizing the importance of thaw layer dynamics in mixing and damping the melt signal. By using the model conceptualization of spatially and temporally variable storage, this study demonstrates the ability of tracer-aided modelling to capture thaw layer dynamics that cause mixing and damping of the isotopic melt signal.
Original languageEnglish
Pages (from-to)2507-2523
Number of pages17
JournalHydrology and Earth System Sciences
Volume23
Issue number6
Early online date3 Jun 2019
DOIs
Publication statusPublished - Jun 2019

Fingerprint

permafrost
tracer
catchment
runoff
frozen ground
modeling
melt
isotope
damping
water
snow water equivalent
cold region
snow accumulation
field capacity
water storage
streamflow
stable isotope
isotopic composition
calibration
simulation

Keywords

  • BLOWING-SNOW
  • DISCONTINUOUS PERMAFROST
  • DISSOLVED ORGANIC-CARBON
  • NORTHWEST-TERRITORIES
  • PEAT PLATEAU
  • SCOTTY CREEK
  • SNOWMELT RUNOFF
  • STABLE-ISOTOPES
  • WOLF CREEK
  • YUKON-TERRITORY

ASJC Scopus subject areas

  • Water Science and Technology
  • Earth and Planetary Sciences (miscellaneous)

Cite this

Spatially distributed tracer-aided runoff modelling and dynamics of storage and water ages in a permafrost-influenced catchment. / Piovano, Thea I.; Tetzlaff, Doerthe (Corresponding Author); Carey, Sean K.; Shatilla, Nadine J.; Smith, Aaron; Soulsby, Christopher.

In: Hydrology and Earth System Sciences, Vol. 23, No. 6, 06.2019, p. 2507-2523.

Research output: Contribution to journalArticle

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abstract = "Permafrost strongly controls hydrological processes in cold regions. Our understanding of how changes in seasonal and perennial frozen ground disposition and linked storage dynamics affect runoff generation processes remains limited. Storage dynamics and water redistribution are influenced by the seasonal variability and spatial heterogeneity of frozen ground, snow accumulation and melt. Stable isotopes are potentially useful for quantifying the dynamics of water sources, flow paths and ages, yet few studies have employed isotope data in permafrost-influenced catchments. Here, we applied the conceptual model STARR (the Spatially distributed Tracer-Aided Rainfall–Runoff model), which facilitates fully distributed simulations of hydrological storage dynamics and runoff processes, isotopic composition and water ages. We adapted this model for a subarctic catchment in Yukon Territory, Canada, with a time-variable implementation of field capacity to include the influence of thaw dynamics. A multi-criteria calibration based on stream flow, snow water equivalent and isotopes was applied to 3 years of data. The integration of isotope data in the spatially distributed model provided the basis for quantifying spatio-temporal dynamics of water storage and ages, emphasizing the importance of thaw layer dynamics in mixing and damping the melt signal. By using the model conceptualization of spatially and temporally variable storage, this study demonstrates the ability of tracer-aided modelling to capture thaw layer dynamics that cause mixing and damping of the isotopic melt signal.",
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