| Climate Of Salt Lake City |
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The Climate of Salt Lake City is widely variable, generally dry, snowy during the winter, and often unpredictable. It consists of four very distinct seasons. As it is located where the Great Basin and the Rocky Mountains come together in a central location, it is influenced by a variety of weather factors. The Pacific Ocean plays a large part, along with the Monsoon s arriving from the south. The low humidity, high elevation, the Great Salt Lake , and the mountains to the east and north (which serve as barriers to Polar High s during the winter) all serve to either moderate or amplify weather effects. TEMPERATURES Winter temperatures are moderated by the Great Salt Lake to the northwest of the city and the Rocky Mountains to the north and east of the state, which serve as barriers to frigid arctic air. However, while Denver does experience the arctic air and has more days with temperatures below 0°F (-18°C), Salt Lake City annually has more days with highs below feezing. Temperatures seldom fall below 0 °F (-18 °C) for any length of time. January is the coldest month in the city, with an average temperature of 29.1 °F (-1.6 °C). Salt Lake City's record low maximum temperature is 2°F (-17°C), set on December 22 , 1990 and its record low temperature is -30 °F (-34 °C), set on February 9 , 1933 . During Spring , temperatures warm up drastically and days are marked by the highest humidity and some of the wildest daily temperature swings of the year. The first summer-like weather usually comes in mid-to-late May. , 2003 , and its record high temperature is 107 °F (41 °C), first set on July 26 , 1960 and again on July 13 , 2002 (although the temperature in 2002 was slightly higher). During Autumn, temperatures drop drastically, with a 50°F (10°C) maximum average temperature drop being experienced within three months. The first winter-like weather is usually experienced in early-to-mid November. Salt Lake City's average yearly temperature is 52.0 °F (11.1 °C), and the freeze-free period lasts an average of 167 days, from April 30 to October 15 . PRECIPITATION Both precipitation and humidity are highest from March through May and lowest from June through mid-September. Major sources of precipitation are winter snow storms originating in the Gulf Of Alaska , late winter and spring rains from the Pineapple Express created in Hawaiian Waters , and summer monsoons from the Gulf Of California . The airport averages 16.50 in (419 mm) of precipitation per year, with bench areas receiving up to 20 inches (500 mm), mainly due to increased snowfall. The airport also averages 58.7 in (1,491 mm) of Snow in a year, which is more than most Great Plains and Mid-Atlantic locations. May is the wettest month, averaging 2.09 in (531 mm) of precipitation. Average year-round humidity is 55%. The summer Monsoon rising from Mexico and Arizona passes through the region beginning in mid-July and continuing into September, bringing intense but short-lived Thunderstorm activity. Tornado es have been known to occur during this time period, the most notable recent example being in 1999 when an F2 tornado struck downtown Salt Lake City, causing extensive damage and resulting in one death. Many of these thunderstorms consist of Dry Lightning , which occurs when humidity is too low to support rainfall and the rain evaporates before reaching the ground. This is the main cause of Wildfire s in Utah during summer. Smoke from such fires in nearby areas sometimes make their way into the valley. Despite the intensity of the thunderstorms, the low humidity, short duration, and isolationism of the thunderstorms all play a part in making this the driest season. July is the driest month, with only 0.72 in (183 mm) of precipitation on average. In late fall, the Pacific Ocean usually begins to kick in again, and starting in late September precipitation begins to increase. During late summer and fall, remnants of Tropical Cyclone s from the East Pacific occasionally reach Utah, resulting in heavy tropical rains. Weather events such as Hail , Freezing Rain , and Sleet are uncommon in Salt Lake City. When they do occur, they are of short duration and rarely accumulate. The record precipitation for a single month occurred in September 1982 , with 7.04 in (179 mm). The record 24 hour precipitation occurred from April 22 - 23 , 1957 , when 2.41 in (61 mm) fell. The first snowfall of the season is usually recorded in late October, although significant snowfall usually does not occur until mid-to-late November. However, snow has been recorded as early as September 17 (in 1965 ). January averages the most snowfall of any month, with 13.6 in (34.5 cm). Snowfall is common through mid-March, but the last snowfall of the season usually occurs in early or mid-April, although snow has been recorded as late as May 18 (in 1977 ). However, significant snow can fall in March and in rare cases even April. Measurable snow falls on average from November 6 through April 18 . The airport averages 58.7 in (149.1 cm) of snow per year, while bench locations near the mountains receive substantially more, reaching 80 to 100 in (200 to 255 cm) annually. These high snowfall totals can be credited to the Lake Effect , in which snow storms passing over the Great Salt Lake are amplified by the warm waters of the lake. The lake effect is usually strongest from mid-fall through mid-winter, when lake waters are warmer and land temperatures are cold enough to support snow. Blizzards are very rare in Salt Lake City, due to a rarity of extreme winds. Although average snowfall is relatively high, large snowstorms of more than about 12 inches (30 cm) are rare. In addition, average winter temperatures in the city are usually not cold enough to support snow cover all winter long. The maximum snow depth recorded in the city was 26 in (66 cm) on January 11 , 1993 . January 1993 was the snowiest month on record, with 50.3 in (128 cm). The record 24 hour snowfall occurred on February 24 - 25 , 1998 , when 18.9 in (48 cm) fell, while the record single storm snowfall occurred from January 6 - 10 , 1993 , with 23.3 in (59 cm). The snowiest season on record was 1951 - 1952 , when 117.3 in (297.9 cm) fell, while the least snowy winter on record was 1939 - 1940 , with 18.5 in (47.0 cm). OTHER WEATHER EVENTS , 1999 (orange fireball is substation exploding)]] The phenomenons El Niño And La Nina also affect precipitation along the Great Basin , bringing occasional cycles of drought and flooding. The largest recent flood in Salt Lake City occurred in 1983 . Triggered by a powerful El Niño, an exceptionally large snowpack caused flooding and massive damage. City Creek burst from its underground diversion and flooded the city. Some streets, such as State Street and 1300 South, were diverted into make-shift rivers to accommodate the overflowing creek. One of the most significant weather event in Salt Lake City occurs in mid-winter, when Temperature Inversion s sometimes form, resulting in cold and extremely foggy, hazy weather in the city while the surrounding mountains enjoy warmer temperatures and sunshine. Temperature inversions are extremely unhealthy and can occur weeks at a time, and are most pronounced in the heart of winter, although may occur in other seasons to a lesser extent. Humidity is only high enough for Fog to occur in winter, although Haze and Smog can be found year-round. Inversions occur when strong areas of high pressure park themselves over the Great Basin . It usually takes a strong storm or Cold Front to force out or break down the high pressure. Tornado es are also relatively uncommon. However, there has been at least one damaging tornado in the city. The Salt Lake City Tornado of August 11 , 1999 , which killed one person and injured 60, resulted in only the second ever fatality from a tornado in Utah, and caused about $500 million in damage. As a result of extended drought patterns, Salt Lake City constructed several reservoirs to hold excess water during flood periods and provide water during drought conditions. Additionally, artesian wells and water siphoned from Utah Lake miles to the south act as alternate water sources for the city. {Link without Title} RECENT WEATHER EVENTS Utah was in a consistent drought from late 1998 through 2004 , although experts warn that the drought-breaking conditions experienced in 2004 and 2005 could actually just be a break in a more extended drought pattern. July of 2002 set the record for the warmest month ever in Salt Lake City, only to be broken in July 2003. 2003 overall was the second warmest year on record, and recorded the second-warmest January, August, and October on record, with the warmest month ever (July). January of 2003 saw a record high January temperature of 63°F (17°C) and record low January snowfall (a trace). That winter was the sixth warmest and third least snowy on record. May 2003 also set a record high May temperature of 99°F (37°C) on two consecutive days. July 2002 also saw a record-tying high temperature of 107°F (41°C), while July 2003 saw a record high minimum temperature (80 °F; 27°C) and a record streak of 100 degree weather (10 days). In late December 2003 a large storm dumped more than 18 inches (460 mm) of snow across the valley, with up to 40 inches (1,000 mm) in high bench areas and up to 100 inches (2,500 mm) in the mountains. From December 25 - 29 , the official station saw 21.9 inches (56 cm). This snowstorm also caused widespread power outages. Accompanied by subsequent snowstorms and a very cold January and February, snow from this storm remained on the ground for the remainder of the winter. From January 3 - 26 , Salt Lake City spent a record amount of time below freezing. January and February were both very cold, but this was followed by the fourth-warmest March on record, which also saw a record-tying March high. Before 2005 , 1998 was the last year to see above-average precipitation. Near record-setting Snowpack in the mountains during the 2004 to 2005 season, as well as heavy spring rains, ended the drought nearly state-wide. Heavy winter and spring rains caused flooding throughout the state. In late January, heavy rains overflowed the Santa Clara River in Washington County in the southwest corner of the state, destroying several homes in Ivins , Santa Clara , and Saint George , and essentially cutting off the small town of Gunlock . Heavy spring rains in late April caused widespread but minor flooding in northern Utah. Snowmelt flooding was a problem in late May and early June, especially along the Sevier River in Garfield and Sevier counties, the Duchesne River in Duchesne and Uintah counties, Coal Creek in Iron County around Cedar City , and the American Fork River in northern Utah County . However, none of this flooding was particularly severe, due to cool temperatures arriving at an opportune time to slow the Snowmelt . REFERENCES
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