While many people view an extensive snow cover as an inconvenience, the winter snow that piles up across the northern portion of the nation and the mountains of the West is important for water management. According to a fact sheet supplied by NOAA's National Snow and Ice Data Center (NSIDC), the mountain snowpack in the West contributes up to 75 percent of that region's annual surface water supply. In this discussion, the term snow cover refers to the areal extent of the snow on the ground, whereas the term snowpack denotes the accumulation of snow especially over mountainous terrain.
For more than a century weather observers have measured and reported snowfall, the liquid water equivalent of the snow, and the depth of the snow on a daily basis. These observations are made not only at the various weather stations operated by the National Weather Service, but also by thousands of volunteer cooperative observers. They measure the depth of newly fallen snow once daily at a particular time (usually 1200 UTC or 7:00 a.m. EST). These observers also melt this snow to determine the liquid water equivalent of the snow. They also measure the average depth of the snow cover, taken at several representative locations. A link to current snowfall and snow depth information can be obtained from the DataStreme WES website. The 24-hour snowfall and the snow depth (in inches) as observed at 1200 UTC are made available by NOAA's Climate Prediction Center. These data are available in several formats, including plots on individual state maps or the entire nation.
In some areas of the country, especially in the West, teams of observers conduct snow surveys to determine the water content of the snowpack in the mountains. However, over the last several years, automated weather stations have been deployed in remote regions to determine the snowfall and other weather conditions that affect the snowpack. The Natural Resources Conservation Service (NRCS), formerly known as the Soil Conservation Service (SCS), maintains a network of at least 600 automated stations across the West (including Alaska) called the SNOTEL Network (SNOTEL=SNOw TELemetry). These remote unattended sites have instruments that measure the water equivalent of snow and other data, and then transmit the collected data to a centralized location, often via satellite relay. One of the quantities plotted is the snow water content, expressed as a percentage of long-term average conditions. The current water equivalent of the snowpack chart produced by the SNOTEL network is available on the DataStreme WES website. These charts are updated daily at approximately 1600 UTC (8:00 a.m. PST).
As of the start of this week (11 March 2007), many of the SNOTEL sites across the West had average or below average water content in the snow pack. Some of the sites in California's high Sierra, across Nevada, eastern Oregon, Utah and Arizona reported between one-half and three-quarters of their typical snow water content. However, SNOTEL sites along the Cascades of Washington State and Oregon, as well as across the central and southern Rockies in Colorado and New Mexico had average to above average values. The distribution of percentages of water content of the snowpack from average is also reflected in the corresponding percentage map of equivalent precipitation totals that include rain as well as melted snow (not shown here) collected at these SNOTEL sites. During the current winter season to date, the northward track of storm systems brought snow to the northern Cascades, but little precipitation to the Sierra and the Southwest. Several major storms that hit the southern and central Rockies helped contribute to the snowpack across Colorado and New Mexico.
For more than 35 years, the fleet of polar-orbiting and geosynchronous satellites has been routinely monitoring the areal extent of snow and ice on a weekly basis. Reflected visible sunlight as well as emitted infrared radiation are used to determine the extent of the snow cover under relatively cloud-free conditions. Microwave radiation is now used to assist the snow cover determination under cloudy skies. Since 1997, NOAA's Satellite Analysis Branch (SAB) of the Satellite Services Division (SSD) produces a daily snow and ice chart with a resolution of 25 km over much of the Northern Hemisphere based upon satellite surveillance, supplemented by surface observations. The current snow cover chart for the continental United States and adjoining portions of Canada and Mexico is found on the DataStreme WES website. White areas depict the snow, while yellow regions show ice cover on the major lakes and bays.
As of the end of last week (10 March 2007), snow covered the northern tier of states from the Dakotas eastward to northern Great Lakes, the higher terrain of the Rockies in Colorado, Wyoming and Utah, along with the Sierra in California and the Cascades in Washington and Oregon. Much of the Northeast, including the Adirondacks of New York State and New England also had an extensive snow cover. Ice was detected in some of the bays along Lakes Superior, Michigan, Huron and Ontario, while Lake Erie and the Gulf of St. Lawrence in eastern Canada were essentially ice covered. Hudson and James Bays in Canada were also ice covered.
Recently, low flying aircraft have been used to monitor the amount of water in snowpack through measurement of upwelling gamma radiation emitted from various radioisotopes that occur naturally in the upper 8 inches of the soil. These aircraft fly along prescribed flight paths at elevations of about 500 feet and at designated times measure the terrestrial gamma radiation. Since snow cover tends to attenuate the gamma radiation in proportion to the amount of water in the snowpack, a comparison of the amount of gamma radiation detected from a flight over a snow cover with that collected over bare ground permits the determination of the snow water equivalent in the snowpack. An operational Airborne Gamma Radiation Snow Survey Program is maintained by the National Operational Hydrologic Remote Sensing Center (NOHRSC) to determine snow water equivalent and soil moisture for NOAA's National Weather Service and the River Forecast Centers. This survey program typically operates from January to April. For example, aircraft surveillance across the Northeast during the exceptionally snowy winter of 2000-01 found that the mountain snowpack in places had a water equivalent of about 12 inches (up to 150% of the long-term average). Such analyses allowed water managers and the public some early guidance in preparing for the spring melt. Flight-line status maps and other information for the current snow season surveys are available.
The NOHRSC produces a variety of national and regional snow analyses that provide daily comprehensive snow information for the continental United States. These current displays include snow cover, snow water content, the average temperature, and several other derived statistics not only for large portions of the nation, but for the watersheds within the areas of responsibility of the individual River Forecast Centers. Individual maps are based upon satellite-derived statistics, supplemented by airborne surveys of the snowpack.
As of the start of this week (11 March 2007), 82 percent of the northern Rockies (western Montana and Idaho) was covered by an average of less than three feet of snow (31.2 inches), with 9 inches of average water equivalent. In contrast, the Southwest (southeastern California and the Four Corners area of southern Utah and Colorado, along with northern sections of New Mexico and Arizona) had only three percent of the region snow covered, with an average snow depth of 0.5 inches and a snow water equivalent of 0.1 inches. In the Northeast (Upstate New York and much of New England), 88 percent of the region had a snow cover, with an average depth of 15.4 inches and an average water content of 3.5 inches.
Return to DataStreme WES Website
Prepared by Edward J. Hopkins, Ph.D., email
hopkins@meteor.wisc.edu
© Copyright, 2007, The American Meteorological Society.
