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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 Wasatch Range (/ ˈ w ɑː s æ tʃ / WAH-satch) or Wasatch Mountains is a mountain range in the western United States that runs about 160 miles (260 km) from the Utah-Idaho border south to central Utah. [1] It is the western edge of the greater Rocky Mountains, and the eastern edge of the Great Basin region. [2]
The Wasatch Front is a semi-arid region at the eastern edge of the Great Basin. The urban corridor mainly lies in zone 7 [5] with minimum average winter temperatures ranging between 0 and 20 °F (−18 and −7 °C) and daytime high temperatures ranging from the mid-30 °F to mid-40 °F range (-1 and 4 °C). Snowfall is common during winter but ...
Lone Peak is a mountain summit in the Wasatch Range southeast of Salt Lake City, Utah, United States, and the center of the Lone Peak Wilderness, established in 1978.With an elevation of 11,260 feet (3,430 m), it is one of the highest peaks in the range and among the most prominent of the Wasatch Front, towering over the Salt Lake City suburb of Draper and easily visible from most of the ...
The Pfeifferhorn is the 11,326 feet (3,452 m) triangularly-shaped peak located in the most isolated part of the Lone Peak Wilderness Area of the Wasatch Mountains in northern Utah, United States. This rugged Utah mountain, commonly referred to as the Little Matterhorn, is the eighth-highest peak in the Wasatch Range. The summit can be reached ...
"As the climate warms, less precipitation falls as snow, and more snow melts during the winter. That decreases snowpack—the amount of snow that accumulates over the winter. Since the 1950s, the snowpack has been decreasing in Utah, as well as Wyoming and Colorado, which contribute snowmelt to the Green and Colorado rivers". [1]
According to the Köppen climate classification system, Wasatch Mountain is located in an alpine subarctic climate zone with long, cold, snowy winters, and cool to warm summers. [6] Due to its altitude, it receives precipitation all year, as snow in winter, and as thunderstorms in summer, with a dry period in late spring.
Snowpack is an accumulation of snow that compresses with time and melts seasonally, often at high elevation or high latitude. [1] [2] Snowpacks are an important water resource that feed streams and rivers as they melt, sometimes leading to flooding. Snowpacks provide water to down-slope communities for drinking and agriculture. [3]