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The Great Salt Lake effect is a small but detectable influence on the local climate and weather around the Great Salt Lake in Utah, United States.In particular, snowstorms are a common occurrence over the region and have major socio-economic impacts due to their significant precipitation amounts.
The Great Salt Lake is the largest saltwater lake in the Western Hemisphere [1] and the eighth-largest terminal lake in the world. [2] It lies in the northern part of the U.S. state of Utah and has a substantial impact upon the local climate , particularly through lake-effect snow .
These include areas east of the Great Lakes in North America, the west coasts of northern Japan, Lake Baikal in Russia, and areas near the Great Salt Lake, Black Sea, Caspian Sea, Baltic Sea, Adriatic Sea, the North Sea and more. Lake-effect blizzards are the blizzard-like conditions resulting from lake-effect snow. Under certain conditions ...
On July 3, the lake's average daily surface water elevation was measured as 4,190.1 feet at the U.S. Geological Survey gauge at Saltair Boat Harbor on the southern end of the lake. Last year, on
Several communities across the Great Lakes region are preparing to be blasted by feet of snow as winter weather moves in just as millions of people across the U.S. ring in 2025.
Some areas of the Wasatch Range in the path of the lake-effect receive up to 500 inches (12,700 mm) per year. This micro climate of enhanced snowfall from the Great Salt Lake spans the entire proximity of the lake. The cottonwood canyons adjacent to Salt Lake City are located in the right position to receive more precipitation from the lake. [8]
Some flooding also occurred in 1987, when the Great Salt Lake reached its all-time maximum water level. A 2010 study indicates that this record event occurred during an overlapping period of three prominent climate cycles that are unique in the region. [7] Significant mid-winter temperature inversions often occur in the Salt Lake Valley. These ...
Guardsman Pass (elevation 9,717 feet (2,962 m) [2] is a high mountain pass in the Wasatch Mountains of Utah. The pass is located on the boundaries of the Uinta-Wasatch-Cache National Forest (specifically the portion known as the Wasatch National Forest ) to the west, and the Bonanza Flats backcountry area to the east.