Road Closures Due to El Portal Fire
The Big Oak Flat Road between Crane Flat and the El Portal Road is temporarily closed. There is no access to Yosemite Valley via the Big Oak Flat Road or Highway 120. Tioga Road is open and accessible via Big Oak Flat and Tioga Pass Entrances. More »
Campground Closures Due to Fire
Crane Flat, Bridalveil Creek, and Yosemite Creek Campgrounds are temporarily closed. More »
Yosemite National Park is Open
Yosemite Valley, Glacier Point, and Wawona/Mariposa Grove areas are open and accessible via Highways 140 and 41. Tioga Road is not accessible via Highways 140 and 41 due to a fire.
When you want to know how deep the snow is, do you simply stick a big ruler down in the ground? Well, this image is not far from the real work of Yosemite’s snow surveyors since the late 1920s.
The tool of choice has been the century-old Mount Rose Snow Tube created in 1909 by Dr. James Edward Church to monitor Lake Tahoe’s water level. Surveyors thrust the hollow, aluminum tube into the snowpack until it strikes the ground beneath. This sample, called a snow core, can be used to measure snow depth and water content.
Measurements are collected several times per year at carefully chosen locations called snow courses. A snow course is simply a section of a snow-covered area where several snow core samples are taken at regularly spaced intervals (such as 50 feet), and measurements are averaged. Snow courses are often located at high elevations, in wilderness areas far from plowed roads. To access the snow courses, today’s surveyors often clip on snowshoes or skis and head out over Yosemite’s rugged terrain, just as they did 90 years ago.
Snow surveys are traditionally conducted four to five times per year, on (or near) the first of February, March, April, May, and sometimes June. The April 1 snow survey is expected to show the peak of the seasonal snow pack. The largest April 1 snow survey in Yosemite’s recent history measured a snow depth of 232.9 inches in 1969. The highest water content measured 96 inches in 1983. Other years with very high measurements include 1995, 2005, and 2006. These survey data provide information about mountain snowpack that can be used to identify trends that are valuable for park managers, hydrologists, climatologists, and water resource managers. The snow survey record in Yosemite is especially valuable because it dates back to 1930 for some snow courses, and because surveyors have taken great effort to assure consistency of measurement techniques and location.
In addition to the monthly snow course data, many agencies monitor snow depth and water content using automated sensors. These sensors are usually installed at weather stations in middle and high elevations. The most common automated sensor is the snow pillow, a sensor like a large scale that uses the weight of the snow to estimate its water content. Although automated methods allow great temporal resolution and potential for high accuracy, these techniques are relatively new and do not have long historical records. It is a priority for surveyors to continue traditional snow course surveys in addition to more advanced techniques.
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Did You Know?
In Yosemite Valley, dropping over 594-foot Nevada Fall and then 317-foot Vernal Fall, the Merced River creates what is known as the “Giant Staircase.” Such exemplary stair-step river morphology is characterized by a large variability in river movement and flow, from quiet pools to the dramatic drops of the waterfalls themselves.