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Surface Water Research Group |
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Department of Geological Sciences, University of Colorado, Boulder |
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Surface Water Research Group |
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Department of Geological Sciences, University of Colorado, Boulder |
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Current Students |
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Dave Bedford
Office: Benson Room 225 |
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Ethan Gutmann
Office: Ekeley/CIRES Room W225 |
Dissertation title: Determination of Soil Hydraulic Properties from Remotely Sensed Surface Temperature in Semi-Arid Environments I am a PhD candidate in the Department of Geological Sciences at the University of Colorado, Boulder. My dissertation is looking at the effect of Soil Hydraulic Properties on surface temperature. Soil hydraulic properties are important parameters in climate models, weather prediction, flood forecasting, and aquifer recharge studies. However, the spatial distribution of these properties is very poorly understood. I hope to use the relationship between surface temperatures and soil hydraulic properties to determine hydraulic properties from remotely sensed surface temperatures. |
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Laure Montandon PhD Candidate
Office: Benson Room 255 |
Dissertation title: The impact of ground reflectance on the estimation of the green vegetation fraction from remote sensing data The green vegetation fraction (Fg) is an important parameter used in many applications, including weather forecast and climate models. Fg is estimated using remote sensing measurements to parametrize Fg models. These models are generally simple mixing models between two end-members: soil and vegetation. My goal is to improve the Fg estimate by providing better characterization of the vegetation's background signal, which should include better constrained soil information as well as information on other ground components like litter. |
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Evan Pugh PhD Student
Office: Benson Room 255 |
Dissertation title: TBD I am currently studying the hydrological impact of Lodgepole pine tree die-off induced by Mountain Pine Beetle infestation. My research focuses on recognizing changes in the timetable of annual snowmelt and streamflow attentuation. I hypothesize that decreases in canopy interception and evapotranspiration brought about by tree death will result in more water reaching and staying in the soil and also in increased stream discharge. Also, I theorize that insect-caused tree death's removal of solar radiation shielding (forest canopy) will result in snow melting earlier in the season. |
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