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Earth System Science Data The Data Publishing Journal
https://doi.org/10.5194/essd-2017-112
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 4.0 License.
Peer-reviewed comment
16 Nov 2017
Review status
This discussion paper is a preprint. It is a manuscript under review for the journal Earth System Science Data (ESSD).
Eleven years of mountain weather, snow, soil moisture and stream flow data from the rain-snow transition zone – the Johnston Draw catchment, Reynolds Creek Experimental Watershed and Critical Zone Observatory, USA
Sarah E. Godsey1, Danny Marks2, Patrick R. Kormos2, Mark S. Seyfried2, Clarissa L. Enslin1, Adam H. Winstral5, James P. McNamara3, and Timothy E. Link4 1Department of Geosciences, Idaho State University, Pocatello, Idaho, USA
2USDA Agricultural Research Services, Boise, Idaho, USA
3Department of Geosciences, Boise State University, Boise, Idaho, USA
4Department of Forest, Rangeland, and Fire Sciences, University of Idaho, Moscow, Idaho, USA
5WSL Institute for Snow and Avalanche Research. SLF, Flüelastrasse 11, 7260 Davos Dorf, Switzerland
Abstract. Detailed hydrometeorological data from the rain-to-snow transition zone in mountain regions are limited. As the climate warms, the transition from rain to snow is moving to higher elevations, and these changes are altering the timing of downslope water delivery. To understand how these changes impact hydrological and biological processes in this climatologically sensitive region, detailed observations from the rain-to-snow transition zone are required. We present a complete hydrometeorological dataset for water years 2004 through 2014 for a watershed that spans the rain-to-snow transition zone (doi:10.15482/USDA.ADC/1402076). The Johnston Draw watershed (1.8 km2), ranging from 1497–1869 m in elevation, is a sub-watershed of the Reynolds Creek Experimental Watershed (RCEW) in southwestern Idaho, USA. The dataset includes continuous hourly hydrometeorological variables across a 372 m elevation gradient, on north- and south- facing slopes, including air temperature, relative humidity, and snow depth from 11 sites in the watershed. Hourly measurements of incoming shortwave radiation, precipitation, wind speed and direction, and soil moisture and temperature are available at selected stations. The dataset includes hourly stream discharge measured at the watershed outlet. These data provide the scientific community with a unique dataset useful for forcing and validating models and will allow for better representation and understanding of the complex processes that occur in the rain-to-snow transition zone.

Citation: Godsey, S. E., Marks, D., Kormos, P. R., Seyfried, M. S., Enslin, C. L., Winstral, A. H., McNamara, J. P., and Link, T. E.: Eleven years of mountain weather, snow, soil moisture and stream flow data from the rain-snow transition zone – the Johnston Draw catchment, Reynolds Creek Experimental Watershed and Critical Zone Observatory, USA, Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2017-112, in review, 2017.
Sarah E. Godsey et al.
Sarah E. Godsey et al.

Data sets

Data from: Eleven years of mountain weather, snow, soil moisture and stream flow data from the rain-snow transition zone - the Johnston Draw catchment, Reynolds Creek Experimental Watershed and Critical Zone Observatory, USA. v1.1
S. E. Godsey, D. G., Marks, P. R. Kormos, M. S. Seyfried, C. L. Enslin, J. P. McNamara, and T. E. Link
https://doi.org/10.15482/USDA.ADC/1402076
Sarah E. Godsey et al.

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Short summary
Weather data in mountainous rain-to-snow transition zones are limited, but vital for water resources. We present a 10-year dataset for this zone that includes hourly temperatures, relative humidity, stream flow, snow depth, precipitation, wind speed/direction, solar energy, and soil moisture at 11 stations. Average air temperatures are near freezing eight months each year, so that slight warming may determine whether rain falls instead of snow, affecting water supplies and fire risk.
Weather data in mountainous rain-to-snow transition zones are limited, but vital for water...
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