Articles | Volume 12, issue 1
https://doi.org/10.5194/tc-12-287-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/tc-12-287-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
23 Jan 2018
Research article |
| 23 Jan 2018
Hydrologic flow path development varies by aspect during spring snowmelt in complex subalpine terrain
Institute of Arctic and Alpine Research, University of Colorado,
Boulder, CO 80309, USA
Steven R. Fassnacht
Department of Ecosystem Science and Sustainability, Colorado State
University, Fort Collins, CO 80523, USA
Michael N. Gooseff
Institute of Arctic and Alpine Research, University of Colorado,
Boulder, CO 80309, USA
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Cited
23 citations as recorded by crossref.
- A deep learning hybrid predictive modeling (HPM) approach for estimating evapotranspiration and ecosystem respiration J. Chen et al. 10.5194/hess-25-6041-2021
- Runoff sensitivity to snow depletion curve representation within a continental scale hydrologic model G. Sexstone et al. 10.1002/hyp.13735
- Snowfall Fraction, Cold Content, and Energy Balance Changes Drive Differential Response to Simulated Warming in an Alpine and Subalpine Snowpack K. Jennings & N. Molotch 10.3389/feart.2020.00186
- Applicability evaluation and improvement of different snow evaporation calculation methods in the Great Xing’an mountains Y. Lin et al. 10.1007/s12145-021-00597-3
- The Presence of Hydraulic Barriers in Layered Snowpacks: TOUGH2 Simulations and Estimated Diversion Lengths R. Webb et al. 10.1007/s11242-018-1079-1
- On the hydrological difference between catchments above and below the intermittent‐persistent snow transition H. Harrison et al. 10.1002/hyp.14411
- Laboratory Observations of Preferential Flow Paths in Snow Using Upward-Looking Polarimetric Radar and Hyperspectral Imaging C. Donahue & K. Hammonds 10.3390/rs14102297
- Rain, Snow and Frozen Soil: Open Questions from a Porescale Perspective with Implications for Geohazards I. Baselt & T. Heinze 10.3390/geosciences11090375
- Spatiotemporal Variations in Liquid Water Content in a Seasonal Snowpack: Implications for Radar Remote Sensing R. Bonnell et al. 10.3390/rs13214223
- The Simulation of L-Band Microwave Emission of Frozen Soil during the Thawing Period with the Community Microwave Emission Model (CMEM) S. Lv et al. 10.34133/2022/9754341
- Quantifying contributions of snowmelt water to streamflow using graphical and chemical hydrograph separation S. Miller et al. 10.1002/hyp.13981
- Extending the vadose zone: Characterizing the role of snow for liquid water storage and transmission in streamflow generation R. Webb et al. 10.1002/hyp.14541
- Partitioning snowmelt and rainfall in the critical zone: effects of climate type and soil properties J. Hammond et al. 10.5194/hess-23-3553-2019
- The Spatial and Temporal Variability of Meltwater Flow Paths: Insights From a Grid of Over 100 Snow Lysimeters R. Webb et al. 10.1002/2017WR020866
- Streamflow partitioning and transit time distribution in snow-dominated basins as a function of climate Z. Fang et al. 10.1016/j.jhydrol.2019.01.029
- Hydrologic connectivity at the hillslope scale through intra‐snowpack flow paths during snowmelt R. Webb et al. 10.1002/hyp.13686
- Advanced monitoring of soil-vegetation co-dynamics reveals the successive controls of snowmelt on soil moisture and on plant seasonal dynamics in a mountainous watershed B. Dafflon et al. 10.3389/feart.2023.976227
- Two-dimensional liquid water flow through snow at the plot scale in continental snowpacks: simulations and field data comparisons R. Webb et al. 10.5194/tc-15-1423-2021
- Investigating Microtopographic and Soil Controls on a Mountainous Meadow Plant Community Using High‐Resolution Remote Sensing and Surface Geophysical Data N. Falco et al. 10.1029/2018JG004394
- Insights Into Preferential Flow Snowpack Runoff Using Random Forest F. Avanzi et al. 10.1029/2019WR024828
- Within‐Stand Boundary Effects on Snow Water Equivalent Distribution in Forested Areas R. Webb et al. 10.1029/2019WR024905
- Hydrological behaviour of an ice‐layered snowpack in a non‐mountainous environment A. Paquotte & M. Baraer 10.1002/hyp.14433
- Combining Ground‐Penetrating Radar With Terrestrial LiDAR Scanning to Estimate the Spatial Distribution of Liquid Water Content in Seasonal Snowpacks R. Webb et al. 10.1029/2018WR022680
22 citations as recorded by crossref.
- A deep learning hybrid predictive modeling (HPM) approach for estimating evapotranspiration and ecosystem respiration J. Chen et al. 10.5194/hess-25-6041-2021
- Runoff sensitivity to snow depletion curve representation within a continental scale hydrologic model G. Sexstone et al. 10.1002/hyp.13735
- Snowfall Fraction, Cold Content, and Energy Balance Changes Drive Differential Response to Simulated Warming in an Alpine and Subalpine Snowpack K. Jennings & N. Molotch 10.3389/feart.2020.00186
- Applicability evaluation and improvement of different snow evaporation calculation methods in the Great Xing’an mountains Y. Lin et al. 10.1007/s12145-021-00597-3
- The Presence of Hydraulic Barriers in Layered Snowpacks: TOUGH2 Simulations and Estimated Diversion Lengths R. Webb et al. 10.1007/s11242-018-1079-1
- On the hydrological difference between catchments above and below the intermittent‐persistent snow transition H. Harrison et al. 10.1002/hyp.14411
- Laboratory Observations of Preferential Flow Paths in Snow Using Upward-Looking Polarimetric Radar and Hyperspectral Imaging C. Donahue & K. Hammonds 10.3390/rs14102297
- Rain, Snow and Frozen Soil: Open Questions from a Porescale Perspective with Implications for Geohazards I. Baselt & T. Heinze 10.3390/geosciences11090375
- Spatiotemporal Variations in Liquid Water Content in a Seasonal Snowpack: Implications for Radar Remote Sensing R. Bonnell et al. 10.3390/rs13214223
- The Simulation of L-Band Microwave Emission of Frozen Soil during the Thawing Period with the Community Microwave Emission Model (CMEM) S. Lv et al. 10.34133/2022/9754341
- Quantifying contributions of snowmelt water to streamflow using graphical and chemical hydrograph separation S. Miller et al. 10.1002/hyp.13981
- Extending the vadose zone: Characterizing the role of snow for liquid water storage and transmission in streamflow generation R. Webb et al. 10.1002/hyp.14541
- Partitioning snowmelt and rainfall in the critical zone: effects of climate type and soil properties J. Hammond et al. 10.5194/hess-23-3553-2019
- The Spatial and Temporal Variability of Meltwater Flow Paths: Insights From a Grid of Over 100 Snow Lysimeters R. Webb et al. 10.1002/2017WR020866
- Streamflow partitioning and transit time distribution in snow-dominated basins as a function of climate Z. Fang et al. 10.1016/j.jhydrol.2019.01.029
- Hydrologic connectivity at the hillslope scale through intra‐snowpack flow paths during snowmelt R. Webb et al. 10.1002/hyp.13686
- Advanced monitoring of soil-vegetation co-dynamics reveals the successive controls of snowmelt on soil moisture and on plant seasonal dynamics in a mountainous watershed B. Dafflon et al. 10.3389/feart.2023.976227
- Two-dimensional liquid water flow through snow at the plot scale in continental snowpacks: simulations and field data comparisons R. Webb et al. 10.5194/tc-15-1423-2021
- Investigating Microtopographic and Soil Controls on a Mountainous Meadow Plant Community Using High‐Resolution Remote Sensing and Surface Geophysical Data N. Falco et al. 10.1029/2018JG004394
- Insights Into Preferential Flow Snowpack Runoff Using Random Forest F. Avanzi et al. 10.1029/2019WR024828
- Within‐Stand Boundary Effects on Snow Water Equivalent Distribution in Forested Areas R. Webb et al. 10.1029/2019WR024905
- Hydrological behaviour of an ice‐layered snowpack in a non‐mountainous environment A. Paquotte & M. Baraer 10.1002/hyp.14433
Latest update: 29 Nov 2023
Short summary
We observed how snowmelt is transported on a hillslope through multiple measurements of snow and soil moisture across a small headwater catchment. We found that snowmelt flows through the snow with less infiltration on north-facing slopes and infiltrates the ground on south-facing slopes. This causes an increase in snow water equivalent at the base of the north-facing slope by as much as 170 %. We present a conceptualization of flow path development to improve future investigations.
We observed how snowmelt is transported on a hillslope through multiple measurements of snow and...
