Articles | Volume 17, issue 1
https://doi.org/10.5194/hess-17-341-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/hess-17-341-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
29 Jan 2013
Research article |
| 29 Jan 2013
Parameterizing sub-surface drainage with geology to improve modeling streamflow responses to climate in data limited environments
C. L. Tague
University of California, Santa Barbara, USA
J. S. Choate
University of California, Santa Barbara, USA
G. Grant
USDA Forest Service, Pacific Northwest Research Station, Corvallis, Oregon, USA
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- Simulation of Dissolved Organic Carbon Flux in the Penobscot Watershed, Maine S. Rouhani et al. 10.1016/j.ecohyd.2021.02.005
- Hydrologic landscape classification evaluates streamflow vulnerability to climate change in Oregon, USA S. Leibowitz et al. 10.5194/hess-18-3367-2014
- Assessing the Impact of Parameter Uncertainty on Modeling Grass Biomass Using a Hybrid Carbon Allocation Strategy J. Reyes et al. 10.1002/2017MS001022
- Fuels treatment and wildfire effects on runoff from Sierra Nevada mixed‐conifer forests P. Saksa et al. 10.1002/eco.2151
- The Counteracting Effects of Snowmelt Rate and Timing on Runoff T. Barnhart et al. 10.1029/2019WR026634
- Snow drought reduces water transit times in headwater streams C. Segura 10.1002/hyp.14437
- Understanding the roles of climate change, land use and land cover change and water diversion project in modulating water- and carbon-use efficiency in Han River Basin F. Yue et al. 10.1016/j.jenvman.2024.123445
- Effect of Tree-to-Shrub Type Conversion in Lower Montane Forests of the Sierra Nevada (USA) on Streamflow R. Bart et al. 10.1371/journal.pone.0161805
- Spatiotemporal dynamics of water sources in a mountain river basin inferred throughδ2Handδ18Oof water L. McGill et al. 10.1002/hyp.14063
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