Abstract
The SNOTEL network is composed of over 800 automated data collection sites located in remote, high-elevation mountain watersheds in the western U.S. They are used to monitor snowpack, precipitation, temperature, and
other climatic conditions. The data collected at SNOTEL sites are transmitted to a central database,
called the Water and Climate Information System, where they are used for water supply forecasting, maps, and reports.
SNOTEL sites are designed to operate unattended and without maintenance for a year or more. A typical SNOTEL remote site
consists of measuring devices and sensors, an equipment shelter for the radio telemetry equipment, and an antenna that
also supports the solar panels used to keep batteries charged. A standard sensor configuration includes a snow pillow,
a storage precipitation gage, and a temperature sensor. The snow pillow measures how much water is in the snowpack by
weighing the snow with a pressure transducer. Devices in the shelter convert the weight of the snow into the snow's
water equivalent -- that is, the actual amount of water in a given volume of snow. SNOTEL stations also collect data on
snow depth, all-season precipitation accumulation, and air temperature with daily maximums, minimums, and averages.
Many enhanced SNOTEL sites are equipped to take soil moisture and soil temperature measurements at various depths,
as well as solar radiation, wind speed, and relative humidity. The configuration at each site is tailored to the physical
conditions, the climate, and the specific requirements of the data users.
The data collected at SNOTEL sites are generally reported multiple times per day, with some sensors reporting hourly