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EspañolLAKE-EFFECT SNOW
(Redirected from Lake effect snow)
'Lake-effect snow', which can be a type of snowsquall, is produced in the winter when cold, arctic winds move across long expanses of warmer lake water, providing energy and picking up water vapor which freezes and is deposited on the lee shores. This effect is enhanced when the moving air mass is uplifted by the orographic effect of higher elevations on the downwind shores. This uplifting can produce narrow, but very intense bands of precipitation, which deposit at a rate of many inches of snow each hour and often bringing copious snowfall totals. The areas affected by lake-effect snow are called snowbelts. This effect occurs in many locations throughout the world, mostly in the Northern Hemisphere, but is best known in the populated areas of the Great Lakes of North America.
If the air temperature is not low enough to keep the precipitation frozen, it falls as lake-effect rain. In order for lake-effect rain or snow to form, the air moving across the lake must be cooler than the surface air (which is likely to be near the temperature of the water surface). Specifically, the air temperature at the altitude where the air pressure is 850 mb should be 13°C lower than the temperature of the air at the surface. Lake-effect occurring when the air at 850 mb is much colder than the water surface can produce thundersnow, snow showers accompanied by lightning and thunder (due to the larger amount of energy available from the increased instability).
Even when precipitation is not produced, cold air passing over warmer water may produce cloud cover. Fast moving cold fronts, known as Alberta clippers often cross the Great Lakes. After the passage of a cold front, winds tend to switch to northwest, and a frequent pattern is for a long lasting low to form over the Canadian Maritimes which may pull cold northwestern air across the Great Lakes for a week or more. Since the prevailing winter winds tend to be colder than the water for much of the winter, the southeastern shores of the lakes are almost constantly overcast, leading to the use of the term ''The Great Gray Funk'' as a synonym for winter. These areas allegedly contain populations that suffer from high rates of seasonal affective disorder, a type of psychological depression thought to be caused by lack of light.[1]
Cold winds in the winter typically prevail from the northwest in the Great Lakes region, producing the most dramatic lake-effect snow falls on the east to south shores of the Great Lakes. This lake-effect produces a significant difference between the snow fall on the eastern and western shores of the Great Lakes.
Lake-effect snows on the Tug Hill Plateau (east of Lake Ontario) frequently set the daily records for snowfall in the United States. Syracuse, New York is directly south of the Tug Hill Plateau and receives significant lake-effect snow from Lake Ontario (although less than the Tug Hill Plateau by as much as 200 inches (508 cm)). In fact, Syracuse receives so much snowfall it is often considered the "snowiest" large city in America, averaging 115.6" (293.6 cm) of snow a year. Syracuse has frequently won the "Golden Snowball" award, a NOAA regional contest for greatest annual snowfall among large Upstate New York snowbelt cities. The communities of Redfield in Oswego County and Montague and North Osceola in Lewis County, all on the Tug Hill Plateau, average over 300 inches (762 cm) of snow a winter, with more than 400 inches (1,016 cm) falling during harsh winters. A 24 hour record for the contiguous United States occurred on January 11th-12th 1997 when 77" (196 cm) of snow fell in Montague, a total of 95 inches (241 cm) of snow falling in that storm between the 11th and 14th. ''(Source, National Weather Service, Buffalo.)'' In February, 2007, a prolonged lake-effect snow event left over 100 inches (254 cm) of snow on the Tug Hill Plateau.[2]
Lake-effect snow from the Finger Lakes occurs in upstate New York as well, until those lakes freeze over. The Appalachian Mountains and Atlantic Ocean largely shield New York City and Philadelphia from picking up any lake-effect snow; snow there tends to come from storm systems mixing with cold weather.
Lake Erie produces a similar effect for a zone stretching from the eastern suburbs of Cleveland to Erie to Buffalo, with a southern limit around Pittsburgh. Remnants of lake-effect snows from Lake Erie have been observed to reach Garrett County in western Maryland. Lake Erie has the distinction of being the only great lake to completely freeze during the winter as a result of being very shallow, although this does not happen every winter. Once frozen, the resulting ice cover temporarily alleviates lake-effect snow from originating there.
Another snowbelt is in the Upper Peninsula (UP) of Michigan, near the cities of Houghton, Marquette, and Munising. These areas frequently average over 200 inches (508 cm), and may receive close to 300 inches (762 cm) of snow a year (for comparison, on the western shore, Duluth, Minnesota receives only 77 inches (196 cm)). Lake Superior and Lake Huron rarely freeze due to their size and depth; lake-effect snow can fall continually in the UP and the Ontario, Canada snowbelts during the winter months. Western Michigan and north-central Indiana can get heavy lake-effect snows as winds pass over Lake Michigan and deposit snows over Traverse City, Grand Rapids, Kalamazoo, and South Bend, but these snows abate significantly before Lansing or Fort Wayne, Indiana.
Cities such as Toronto, Hamilton, Detroit, Milwaukee, and Chicago frequently miss out on lake-effect events because they are not on the leeward shore of a lake during a northwest wind. However Toronto and Hamilton are close enough to Georgian Bay and Lake Huron that they receive small amounts of lake-effect snow each winter. Even so, a less frequent easterly or northeasterly wind can deposit heavy snows on Chicago or Milwaukee much as a northwest/westerly wind does for the opposite side of Lake Michigan.
The southern and southeastern sides of the Great Salt Lake receive significant lake-effect snow, locally known as "The Greatest Snow on Earth". Since the Great Salt Lake never freezes, the lake-effect can affect the weather along the Wasatch front year around. The Finger Lakes of New York also are long enough for lake-effect precipitation. The twin cities of Sherman, Texas and Denison, Texas are also known to have experienced lake-effect snow from Lake Texoma in rare instances.
Similar snowfall can occur near large inland bays, where it is known as 'Bay effect snow'. Bay-effect snows fall downwind of Delaware Bay, Chesapeake Bay, and Massachusetts Bay when the basic criteria are met. Ocean effect snows are possible downwind of the Gulf Stream and the Sea of Japan.[3] Canadian Maritimes, in particular Nova Scotia and Prince Edward Island provinces, are often affected by such snowsqualls when an arctic winter airmass moves over unfrozen waters. This effect is especially intense with very warm waters of the Gulf Stream or the Sea of Japan. This also happens usually a couple of times per winter in the area near Cape Cod and on rarer occasions along Long Island. An extreme occurrence of "ocean effect" snow occurred on January 24, 2003, when wind off the Atlantic, combined with air temperatures in the 20 °F (-6.6 °C), brought snow flurries to the Atlantic coast of Florida as far south as Cape Canaveral.[4]
A phenomenon similar to lake-effect snow may also occur in other countries, near large lakes or sea regions. One example is the Aegean Sea in Greece, where cold northeast winds known as the boreas can produce heavy snowfalls over Euvia and Northern parts of Athens. These systems can have a duration of 3 days to 1 week and result snowcover of 40 inches (101.6 cm) or more. Similar effects also occur in the regions of the Black Sea in Georgia and Turkey or the Adriatic Sea and Italy. The snowfall in the eastern regions of the Black Sea is amplified by the orographic effect of the nearby Caucasus Mountains, often resulting in snowfall of several meters, especially at higher elevations. In Norhtern Europe, cold, dry airmasses from Sweden can blow over the Baltic Sea and cause heavy snow squalls on areas of the southern and eastern coasts.
In the United Kingdom, easterly winds bringing cold Continental air across the North Sea can lead to a similar phenomenon. Locally it's also known as "lake-effect snow" despite the snow coming in from the sea rather than a lake. [5]
Due to the North Sea being relatively warm (around 13C at the beginning of winter, typically 10C to 6C by the end), sufficiently cold air aloft can create significant snowfalls in a relatively short period of time. The best-known example occurred in January 1987, when record-breakingly cold air (associated with an upper low) moved across the North Sea towards the UK. The end result was over a foot of snow for coastal areas, leading to communities being cut off for over a week. In recent years lake-effect snow has been much lighter, due to a lack of very cold Continental easterlies.
1. http://www.wunderground.com/health/mood.asp
2. http://www.weather.com/maps/maptype/severeusnational/usextremesnowfall_large.html?from=wxcenter_maps
3. Lake Effect-type Phenomena in Other Regions. by COMET Retrieved on 2006-11-05.
4. National Weather Serivce Office, Melbourne, Florida. Cold Temperatures and Snow Flurries in East-Central Florida January 24, 2003. Retrieved on 2006-11-05.
5. USW archives [1] Retrieved on 2007-08-03.
★ Great Salt Lake effect
Warnings about lake-effect snow:
'United States':
★ Lake Effect Snow Advisory
★ Lake Effect Snow Warning
★ Severe weather terminology (United States)
'Canada':
★ Snowsquall warning
★ Severe weather terminology (Canada)
★ Lake effect forecasting
★ What is lake effect snow?
★ The Golden Snowball Award website
★ Canadian Snowsquall storm chaser
★ Digital Snow Museum
Lake-effect precipitation coming off the Great Lakes, as seen from NEXRAD.
'Lake-effect snow', which can be a type of snowsquall, is produced in the winter when cold, arctic winds move across long expanses of warmer lake water, providing energy and picking up water vapor which freezes and is deposited on the lee shores. This effect is enhanced when the moving air mass is uplifted by the orographic effect of higher elevations on the downwind shores. This uplifting can produce narrow, but very intense bands of precipitation, which deposit at a rate of many inches of snow each hour and often bringing copious snowfall totals. The areas affected by lake-effect snow are called snowbelts. This effect occurs in many locations throughout the world, mostly in the Northern Hemisphere, but is best known in the populated areas of the Great Lakes of North America.
If the air temperature is not low enough to keep the precipitation frozen, it falls as lake-effect rain. In order for lake-effect rain or snow to form, the air moving across the lake must be cooler than the surface air (which is likely to be near the temperature of the water surface). Specifically, the air temperature at the altitude where the air pressure is 850 mb should be 13°C lower than the temperature of the air at the surface. Lake-effect occurring when the air at 850 mb is much colder than the water surface can produce thundersnow, snow showers accompanied by lightning and thunder (due to the larger amount of energy available from the increased instability).
| Contents |
| Cause |
| Phenomenon in Southeast Canada and the U.S Northeast |
| Phenomenon elsewhere in United States |
| Similar phenomena |
| International phenomena |
| References |
| See also |
| External links |
Cause
Lake-effect snow produced as cold winds blow clouds over warm waters.
Even when precipitation is not produced, cold air passing over warmer water may produce cloud cover. Fast moving cold fronts, known as Alberta clippers often cross the Great Lakes. After the passage of a cold front, winds tend to switch to northwest, and a frequent pattern is for a long lasting low to form over the Canadian Maritimes which may pull cold northwestern air across the Great Lakes for a week or more. Since the prevailing winter winds tend to be colder than the water for much of the winter, the southeastern shores of the lakes are almost constantly overcast, leading to the use of the term ''The Great Gray Funk'' as a synonym for winter. These areas allegedly contain populations that suffer from high rates of seasonal affective disorder, a type of psychological depression thought to be caused by lack of light.[1]
Phenomenon in Southeast Canada and the U.S Northeast
Cold winds in the winter typically prevail from the northwest in the Great Lakes region, producing the most dramatic lake-effect snow falls on the east to south shores of the Great Lakes. This lake-effect produces a significant difference between the snow fall on the eastern and western shores of the Great Lakes.
Lake-effect snows on the Tug Hill Plateau (east of Lake Ontario) frequently set the daily records for snowfall in the United States. Syracuse, New York is directly south of the Tug Hill Plateau and receives significant lake-effect snow from Lake Ontario (although less than the Tug Hill Plateau by as much as 200 inches (508 cm)). In fact, Syracuse receives so much snowfall it is often considered the "snowiest" large city in America, averaging 115.6" (293.6 cm) of snow a year. Syracuse has frequently won the "Golden Snowball" award, a NOAA regional contest for greatest annual snowfall among large Upstate New York snowbelt cities. The communities of Redfield in Oswego County and Montague and North Osceola in Lewis County, all on the Tug Hill Plateau, average over 300 inches (762 cm) of snow a winter, with more than 400 inches (1,016 cm) falling during harsh winters. A 24 hour record for the contiguous United States occurred on January 11th-12th 1997 when 77" (196 cm) of snow fell in Montague, a total of 95 inches (241 cm) of snow falling in that storm between the 11th and 14th. ''(Source, National Weather Service, Buffalo.)'' In February, 2007, a prolonged lake-effect snow event left over 100 inches (254 cm) of snow on the Tug Hill Plateau.[2]
Lake Erie produces a similar effect for a zone stretching from the eastern suburbs of Cleveland to Erie to Buffalo, with a southern limit around Pittsburgh. Remnants of lake-effect snows from Lake Erie have been observed to reach Garrett County in western Maryland. Lake Erie has the distinction of being the only great lake to completely freeze during the winter as a result of being very shallow, although this does not happen every winter. Once frozen, the resulting ice cover temporarily alleviates lake-effect snow from originating there.
Visible Satellite image showing a large single lake-effect band with vigorous vertical motion. This band produced 8 inches (20 cm) of snow in the eastern and northern suburbs of Toronto.
Cities such as Toronto, Hamilton, Detroit, Milwaukee, and Chicago frequently miss out on lake-effect events because they are not on the leeward shore of a lake during a northwest wind. However Toronto and Hamilton are close enough to Georgian Bay and Lake Huron that they receive small amounts of lake-effect snow each winter. Even so, a less frequent easterly or northeasterly wind can deposit heavy snows on Chicago or Milwaukee much as a northwest/westerly wind does for the opposite side of Lake Michigan.
Phenomenon elsewhere in United States
Fulton, New York after a snowburst dropped 4-6 feet of snow over most of Oswego County between January 28-31, 2004.
The southern and southeastern sides of the Great Salt Lake receive significant lake-effect snow, locally known as "The Greatest Snow on Earth". Since the Great Salt Lake never freezes, the lake-effect can affect the weather along the Wasatch front year around. The Finger Lakes of New York also are long enough for lake-effect precipitation. The twin cities of Sherman, Texas and Denison, Texas are also known to have experienced lake-effect snow from Lake Texoma in rare instances.
Similar phenomena
Similar snowfall can occur near large inland bays, where it is known as 'Bay effect snow'. Bay-effect snows fall downwind of Delaware Bay, Chesapeake Bay, and Massachusetts Bay when the basic criteria are met. Ocean effect snows are possible downwind of the Gulf Stream and the Sea of Japan.[3] Canadian Maritimes, in particular Nova Scotia and Prince Edward Island provinces, are often affected by such snowsqualls when an arctic winter airmass moves over unfrozen waters. This effect is especially intense with very warm waters of the Gulf Stream or the Sea of Japan. This also happens usually a couple of times per winter in the area near Cape Cod and on rarer occasions along Long Island. An extreme occurrence of "ocean effect" snow occurred on January 24, 2003, when wind off the Atlantic, combined with air temperatures in the 20 °F (-6.6 °C), brought snow flurries to the Atlantic coast of Florida as far south as Cape Canaveral.[4]
International phenomena
Chart showing the lake-effect snow event of Jaunary 1987 in the UK. A continuous stream of showers deposited over a foot of snow over SE coastal regions.
A phenomenon similar to lake-effect snow may also occur in other countries, near large lakes or sea regions. One example is the Aegean Sea in Greece, where cold northeast winds known as the boreas can produce heavy snowfalls over Euvia and Northern parts of Athens. These systems can have a duration of 3 days to 1 week and result snowcover of 40 inches (101.6 cm) or more. Similar effects also occur in the regions of the Black Sea in Georgia and Turkey or the Adriatic Sea and Italy. The snowfall in the eastern regions of the Black Sea is amplified by the orographic effect of the nearby Caucasus Mountains, often resulting in snowfall of several meters, especially at higher elevations. In Norhtern Europe, cold, dry airmasses from Sweden can blow over the Baltic Sea and cause heavy snow squalls on areas of the southern and eastern coasts.
In the United Kingdom, easterly winds bringing cold Continental air across the North Sea can lead to a similar phenomenon. Locally it's also known as "lake-effect snow" despite the snow coming in from the sea rather than a lake. [5]
Due to the North Sea being relatively warm (around 13C at the beginning of winter, typically 10C to 6C by the end), sufficiently cold air aloft can create significant snowfalls in a relatively short period of time. The best-known example occurred in January 1987, when record-breakingly cold air (associated with an upper low) moved across the North Sea towards the UK. The end result was over a foot of snow for coastal areas, leading to communities being cut off for over a week. In recent years lake-effect snow has been much lighter, due to a lack of very cold Continental easterlies.
References
1. http://www.wunderground.com/health/mood.asp
2. http://www.weather.com/maps/maptype/severeusnational/usextremesnowfall_large.html?from=wxcenter_maps
3. Lake Effect-type Phenomena in Other Regions. by COMET Retrieved on 2006-11-05.
4. National Weather Serivce Office, Melbourne, Florida. Cold Temperatures and Snow Flurries in East-Central Florida January 24, 2003. Retrieved on 2006-11-05.
5. USW archives [1] Retrieved on 2007-08-03.
See also
★ Great Salt Lake effect
Warnings about lake-effect snow:
'United States':
★ Lake Effect Snow Advisory
★ Lake Effect Snow Warning
★ Severe weather terminology (United States)
'Canada':
★ Snowsquall warning
★ Severe weather terminology (Canada)
External links
★ Lake effect forecasting
★ What is lake effect snow?
★ The Golden Snowball Award website
★ Canadian Snowsquall storm chaser
★ Digital Snow Museum
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