Great Salt Lake effect

Great Salt Lake effect

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 never freezes and can warm rapidly which allows lake-effect precipitation to occur from September through May. Lake-enhanced snowstorms are often attributed to creating what is locally known as "The Greatest Snow on Earth."

Lake enhancement

Lake-effect snow around the Great Salt Lake is generated in a similar fashion to elsewhere in the world. For the Great Salt Lake, lake enhanced precipitation occurs when a strong, cold, northwesterly wind blows across a relatively warm lake. This is common after a cold front passage, where the winds are predominantly northwesterly and the air is much colder than the lake. When the land-lake breeze blows towards the lake, there is a convergence zone that acts to channel the cold air over the center of the lake and further enhance precipitation. The salinity of the Great Salt Lake prevents freezing but reduces the saturation vapor pressure and latent heat flux into the overlying air. As a result, minimal amounts of moisture and latent heat are added to the air moving over the lake. The Great Salt Lake primarily provides a lifting mechanism and acts as an atmospheric destabilizer, which encourages convection. This is in contrast to the Great Lakes, where the lakes contribute significant amounts of moisture and latent heat. The high relief of the Wasatch mountains further capitalizes on lake enhancement and can receive multiple feet of snow from lake-effect alone.

Forecasting lake-effect snow

Accurate prediction of snowstorms developing in the lee of the great Salt Lake is one of the major forecast challenges facing northern Utah. Forecasting skill has drastically improved in recent years due to a better observational network including the NEXRAD radar system. An accurate forecast involves identifying the crucial requirements for lake-effect precipitation. The basic requirements are a conditionally unstable environment, significant moisture and a lifting mechanism. Many different variables go into these requirements. Through extensive analyses and field experiments the understanding of lake-effect snowstorms has improved drastically in recent years. Many general rules of thumb have been developed in order to predict the occurrence, location and severity of lake-effect snow.

Rules of thumb

*A strong Northwesterly flow maximizes precipitation for the Salt Lake Valley.
*A minimal temperature difference of 16°C between the surface and 700 mbar is needed - but not necessarily sufficient in itself to cause lake-effect snow.
*An inversion or stable layer below 700mb has never yielded lake-effect snow.
*Lake-effect snow can occur in concert with synoptic scale storm systems.
*A large lake-land temperature difference favors over-lake convergence.
*Lake-effect is typically initiated during the night when land-breeze convergence is favored and convection occurs predominantly over the lake.
*During the daytime lake-effect precipitation dissipates when solar heating creates scattered widespread convection over the land.
*The 700mb winds typically determine the geographic position of the precipitation
*Limited amounts of directional and vertical wind shear tend to produce heavier precipitation events.
*The Great Salt Lake contributes minimal amounts of moisture so that upstream moisture is a crucial variable.

References

* Carpenter, D. M., 1993: The lake-effect of the Great Salt Lake: Overview and forecast problems. Wea. Forecasting, 8, 181-193.

*Steenburgh, W. J., S. F. Halvorson, and D. J. Onton, 2000: Climatology of lake-effect snowstorms of the Great Salt Lake. Mon. Wea. Rev. , 128, 709-727

*Steenburgh, W. J, 1999: Lake Effect of the Great Salt Lake: Scientific Overview and Forecast Diagnostics. http://www.met.utah.edu/jimsteen/cirp/lake_diagnostics/


Wikimedia Foundation. 2010.

Игры ⚽ Нужно решить контрольную?

Look at other dictionaries:

  • Great Salt Lake — Infobox lake lake name = Great Salt Lake image lake = Great Salt Lake ISS 2003.jpg caption lake = Satellite photo in summer 2003 after five years of drought, reaching near record lows. image bathymetry = caption bathymetry = location = Utah,… …   Wikipedia

  • Lake-effect snow — Lake Effect redirects here. For the American literary journal, see Lake Effect (journal). Lake effect precipitation coming off Lake Erie and into Western New York, as seen by NEXRAD radar, October 12–13, 2006 …   Wikipedia

  • Salt Lake City, Utah — Infobox Settlement official name = City of Salt Lake City settlement type = City nickname = Crossroads of the West, Salt Lake, SLC imagesize = image caption = Downtown Salt Lake City in April 2008 image mapsize = 250px map caption = Location of… …   Wikipedia

  • Salt Lake County, Utah — Infobox U.S. County county = Salt Lake County state = Utah seal seallink map size = 150 founded year = 1852 seat wl = Salt Lake City largest city wl = Salt Lake City area total sq mi = 808 area total km2 = 2092 area land sq mi = 737 area land km2 …   Wikipedia

  • Climate of Salt Lake City — Salt Lake City Climate chart (explanation) J F M A M J J A S O …   Wikipedia

  • Great Bitter Lake — Infobox lake lake name = Great Bitter Lake image lake = Great Bitter Lake from space (hires).jpg caption lake = image bathymetry = caption bathymetry = location = coords = coord|30|20|N|32|23|E|region:EG type:waterbody|display=inline,title type …   Wikipedia

  • lake — lake1 /layk/, n. 1. a body of fresh or salt water of considerable size, surrounded by land. 2. any similar body or pool of other liquid, as oil. 3. (go) jump in the lake, (used as an exclamation of dismissal or impatience.) [bef. 1000; ME lak(e) …   Universalium

  • Lake — /layk/, n. Simon, 1866 1945, U.S. engineer and naval architect. * * * I Relatively large body of slow moving or standing water that occupies an inland basin. Lakes are most abundant in high northern latitudes and in mountain regions, particularly …   Universalium

  • salt — salt1 saltlike, adj. /sawlt/, n. 1. a crystalline compound, sodium chloride, NaCl, occurring as a mineral, a constituent of seawater, etc., and used for seasoning food, as a preservative, etc. 2. table salt mixed with a particular herb or… …   Universalium

  • SALT — /sawlt/, n. See Strategic Arms Limitation Talks. * * * I Chemical compound formed when the hydrogen of an acid is replaced by a metal or its equivalent, such as ammonium (NH4). Typically, an acid and a base react to form a salt and water. Most… …   Universalium

Share the article and excerpts

Direct link
Do a right-click on the link above
and select “Copy Link”