Clarissa Enslin
GRAD STUDENT
MS Geology
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Reynolds MS Student, Idaho State University
BS, Geology, California University of Pennsylvannia, 2014
I will be utilizing the ISNOBAL model to model snowmelt and wind-induced snow redistribution in a sub-watershed of the Reynolds Creek Experimental Watershed. ISNOBAL is a spatially-distributed energy balance snowmelt model that simulates snow-cover development and ablation from images of distributed meteorological forcing variables. The project is part of the WC-WAVE and is funded by EPSCoR.
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CZO Publications
Papers/Books
2018
Eleven years of mountain weather, snow, soil moisture and streamflow data from the rain–snow transition zone – the Johnston Draw catchment, Reynolds Creek Experimental Watershed and Critical Zone Observatory, USA. Godsey, S. E., Marks, D., Kormos, P. R., Seyfried, M. S., Enslin, C. L., Winstral, A. H., McNamara, J. P., and Link, T. E. (2018): Earth Syst. Sci. Data, 10, 1207-1216
Papers and books that explicitly acknowledge a CZO grant are highlighted in PALE ORANGE.
Other CZO Publications
2018
Eleven years of mountain weather, snow, soil moisture and streamflow data from the rain–snow transition zone – the Johnston Draw catchment, Reynolds Creek Experimental Watershed and Critical Zone Observatory, USA. Godsey, S. E., Marks, D., Kormos, P. R., Seyfried, M. S., Enslin, C. L., Winstral, A. H., McNamara, J. P., and Link, T. E. (2018): Earth Syst. Sci. Data, 10, 1207-1216
2016
Understanding the rain-to-snow transition zone: modeling snowmelt and the spatial distribution of water resources in southwestern Idaho. Enslin, C. (2016): Idaho State University
2015
ISNOBAL: Impacts of Extreme Precipitation event in the rain-snow transition. Enslin, C., Marks, D., Godsey, S., and P. Kormos (2015): Summer Tri-State EPSCoR Meeting
2015
A hydrometeorological dataset across the rain-to-snow transition at Reynolds Creek Critical Zone Observatory, Idaho. Enslin, C., Marks, D., Godsey, S., Kormos, P., Seyfried, M., and T. Link (2015): American Geophysical Union Fall Meeting
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