Articles | Volume 24, issue 11
https://doi.org/10.5194/hess-24-5095-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/hess-24-5095-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| Highlight paper
| 
05 Nov 2020
Research article | Highlight paper |
| 05 Nov 2020
| 05 Nov 2020
The pulse of a montane ecosystem: coupling between daily cycles in solar flux, snowmelt, transpiration, groundwater, and streamflow at Sagehen Creek and Independence Creek, Sierra Nevada, USA
Department of Earth and Planetary Science, University of California,
Berkeley, California, USA
Department of Environmental Systems Science, ETH Zurich, Zurich,
Switzerland
Swiss Federal Research Institute WSL, Birmensdorf, Switzerland
Sarah E. Godsey
Department of Earth and Planetary Science, University of California,
Berkeley, California, USA
Department of Geosciences, Idaho State University, Pocatello, Idaho,
USA
Madeline Solomon
Department of Geography, University of California, Berkeley,
California, USA
Randall Osterhuber
Central Sierra Snow Laboratory, Norden, California, USA
Joseph R. McConnell
Division of Hydrological Sciences, Desert Research Institute, Reno,
Nevada, USA
Daniele Penna
Department of Environmental Systems Science, ETH Zurich, Zurich,
Switzerland
Department of Agriculture, Food, Environment and Forestry, University
of Florence, Florence, Italy
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24 citations as recorded by crossref.
- Shallow-groundwater-level time series and a groundwater chemistry survey from a boreal headwater catchment, Krycklan, Sweden J. Erdbrügger et al. 10.5194/essd-15-1779-2023
- Towards a hydrogeomorphological understanding of proglacial catchments: an assessment of groundwater storage and release in an Alpine catchment T. Müller et al. 10.5194/hess-26-6029-2022
- Temporal and spatial diurnal dynamics of the hysteresis of weighed transpiration and water transport in tomatoes L. Ma et al. 10.1016/j.envexpbot.2023.105238
- Linking between Water Use Efficiency and Leaf Area Index Along an Aridity Gradient in Dryland Forests M. Dubinin et al. 10.2139/ssrn.4124944
- Inferring Hillslope Groundwater Recharge Ratios From the Storage‐Discharge Relation D. Dralle et al. 10.1029/2023GL104255
- Watershed memory amplified the Oroville rain-on-snow flood of February 2017 K. Haleakala et al. 10.1093/pnasnexus/pgac295
- The prediction of uneven snowpack response to forest thinning informs forest restoration in the central Sierra Nevada G. Lewis et al. 10.1002/eco.2580
- Assessing the large-scale plant–water relations in the humid, subtropical Pearl River basin of China H. Wang et al. 10.5194/hess-25-4741-2021
- Riparian zone as a variable source area for the estimation of evapotranspiration through the analysis of daily fluctuations in streamflow M. Sarwar et al. 10.1002/hyp.14708
- Dynamics of evapotranspiration from concurrent above- and below-canopy flux measurements in a montane Sierra Nevada forest S. Wolf et al. 10.1016/j.agrformet.2023.109864
- Diel streamflow cycles suggest more sensitive snowmelt-driven streamflow to climate change than land surface modeling does S. Krogh et al. 10.5194/hess-26-3393-2022
- How do geomorphic characteristics affect the source of tree water uptake in restored river floodplains? M. Engel et al. 10.1002/eco.2443
- Continuous high-frequency pesticide monitoring in a small tile-drained agricultural stream to reveal diel concentration fluctuations in dry periods D. la Cecilia et al. 10.3389/frwa.2022.1062198
- SnowWarp: An open science and open data tool for daily monitoring of snow dynamics G. Laurin et al. 10.1016/j.envsoft.2022.105477
- Water yield response to forest treatment patterns in a sierra nevada watershed K. Smith et al. 10.1016/j.ejrh.2024.101762
- Ecosystem groundwater use enhances carbon assimilation and tree growth in a semi-arid Oak Savanna S. Ruehr et al. 10.1016/j.agrformet.2023.109725
- Satellite-based assessment of water use and leaf area efficiencies of dryland conifer forests along an aridity gradient M. Dubinin et al. 10.1016/j.scitotenv.2023.165977
- Nonlinear Riparian Interactions Drive Changes in Headwater Streamflow S. Newcomb & S. Godsey 10.1029/2023WR034870
- Role of transpiration in modulating ecosystem services in secondary tropical montane forests of Eastern Himalaya in India M. Kumar et al. 10.1016/j.ecohyd.2024.04.001
- A multi‐scale assessment of forest treatment impacts on evapotranspiration and water yield in the Sierra Nevada K. Boden et al. 10.1002/eco.2548
- Resolving streamflow diel fluctuations in a small agricultural catchment with an integrated surface‐subsurface hydrological model D. la Cecilia & M. Camporese 10.1002/hyp.14768
- Near-field variability of evaposublimation in a montane conifer forest S. Drake et al. 10.3389/feart.2023.1249113
- Groundwater‐Mediated Memory of Past Climate Controls Water Yield in Snowmelt‐Dominated Catchments P. Brooks et al. 10.1029/2021WR030605
- Hydrological dynamics of snowmelt induced streamflow in a high mountain catchment of the Pyrenees under contrasting snow accumulation and duration years J. López‐Moreno et al. 10.1002/hyp.15127
4 citations as recorded by crossref.
- Evapotranspiration and groundwater inputs control the timing of diel cycling of stream drying during low-flow periods S. Warix et al. 10.3389/frwa.2023.1279838
- Pulses within pulses: Concentration‐discharge relationships across temporal scales in a snowmelt‐dominated Rocky Mountain catchment R. Hensley et al. 10.1002/hyp.14700
- Influence of groundwater and topography on stream drying in semi‐arid headwater streams S. Warix et al. 10.1002/hyp.14185
- Snowmelt characteristics in a pristine mountain catchment of the Jalovecký Creek, Slovakia, over the last three decades L. Holko et al. 10.1002/hyp.14128
Latest update: 10 May 2024
Short summary
Streams and groundwaters often show daily cycles in response to snowmelt and evapotranspiration. These typically have a roughly 6 h time lag, which is often interpreted as a travel-time lag. Here we show that it is instead primarily a phase lag that arises because aquifers integrate their inputs over time. We further show how these cycles shift seasonally, mirroring the springtime retreat of snow cover to higher elevations and the seasonal advance and retreat of photosynthetic activity.
Streams and groundwaters often show daily cycles in response to snowmelt and evapotranspiration....
