Research article 23 Jan 2018
Research article | 23 Jan 2018
Hydrologic flow path development varies by aspect during spring snowmelt in complex subalpine terrain
Ryan W. Webb et al.
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Cited
13 citations as recorded by crossref.
- Runoff sensitivity to snow depletion curve representation within a continental scale hydrologic model G. Sexstone et al. 10.1002/hyp.13735
- 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
- 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
- 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
- The Presence of Hydraulic Barriers in Layered Snowpacks: TOUGH2 Simulations and Estimated Diversion Lengths R. Webb et al. 10.1007/s11242-018-1079-1
- 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
- Quantifying contributions of snowmelt water to streamflow using graphical and chemical hydrograph separation S. Miller et al. 10.1002/hyp.13981
- 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
- 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
- Spatio-temporal aspects of snowpack runoff formation during rain on snow S. Würzer & T. Jonas 10.1002/hyp.13240
11 citations as recorded by crossref.
- Runoff sensitivity to snow depletion curve representation within a continental scale hydrologic model G. Sexstone et al. 10.1002/hyp.13735
- 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
- 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
- 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
- The Presence of Hydraulic Barriers in Layered Snowpacks: TOUGH2 Simulations and Estimated Diversion Lengths R. Webb et al. 10.1007/s11242-018-1079-1
- 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
- Quantifying contributions of snowmelt water to streamflow using graphical and chemical hydrograph separation S. Miller et al. 10.1002/hyp.13981
- 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
2 citations as recorded by crossref.
Latest update: 02 Mar 2021
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...