Meteorological history | |
---|---|
Formed | November 8,2014 |
Dissipated | November 23,2014 [1] |
Cold wave | |
Lowest temperature | −34.0 °F (−36.7 °C) in Thermopolis,WY on November 14 [2] |
Overall effects | |
Fatalities | At least 30 [3] [4] [5] [note 1] |
Areas affected | Canada Contiguous United States Northern Mexico |
Part of the 2014–15 North American winter |
The November 2014 North American cold wave was an extreme weather event that occurred across most of Canada and the contiguous United States,including parts of the Western United States up to western California. One of the first events of the winter,the cold wave was caused by the northward movement of an extremely powerful bomb cyclone associated with Typhoon Nuri's remnant,which shifted the jet stream far northward,creating an omega block pattern. This allowed a piece of the polar vortex to advance southward into the Central and Eastern United States,bringing record-cold temperatures to much of the region. [6] [7] [8] In contrast,Alaska experienced above-average temperatures.
This was the worst cold wave that the North American region had experienced since an earlier cold wave in early 2014. The cold wave was expected to last for a few weeks,extending at least until American Thanksgiving. [9] Although the Omega Block broke down on November 20,due to a powerful storm moving into the Gulf of Alaska,frigid conditions continued to persist across much of the United States. There was also concern among some meteorologists that another cold wave or abnormally cold trend might persist throughout the winter of 2014–15,the chances of which were "above average." [10] On November 23,a warming trend primarily in the Eastern United States brought an end to the cold wave; [1] however,below-average temperatures were forecast to return to the Midwest by November 24. Despite the development of a second cold wave,it ended on December 6,when a ridge of high pressure brought above-average temperatures to the region,especially in the Central United States.
On November 8, the northward movement of a bomb cyclone associated with Typhoon Nuri's remnants shifted the jet stream far to the north, creating an omega block pattern, which allowed a fragment of the polar vortex to descend from Arctic region into lower Canada and the Eastern United States, affecting up to 200 million people with colder-than-normal temperatures and early snowstorms. Although the Omega block broke down on November 20, a powerful storm brought more frigid temperatures. The wave ended on December 6 when an area of high pressure moved in. [11]
Some meteorologists also predicted that the winter of 2014–15 would be abnormally cold across the Eastern United States (though on October 16 the NOAA predicted warmer than average winter temperatures in the Northeast [12] ), due to early snowfall in Siberia, and a weak but developing El Niño, which are both factors in erratic jet stream behavior that could lead to an abnormally cold winter. [10] That prediction turned out to be very accurate, and 2014-15 was indeed a very cold winter in the Northeast.
November 18 was the coldest November morning since 1976 with a national average temperature of 19.4 °F (−7.0 °C) and below-freezing temperatures reported in all 50 states. On that date, Joplin set a record low for the entire month of November, at 6 °F (−14 °C). Houston had its earliest fall freeze since 1999, and Kansas City also dipped down to 6 °F (−14 °C). In Boise, a record low of 5 °F (−15 °C) was established. Paducah set a record low of 10 °F (−12 °C), Evansville dipped down to 9 °F (−13 °C), and Cape Girardeau, Missouri got down to 8 °F (−13 °C). [13] Some U.S. locations had temperatures 45 °F (25 °C) below normal. Sub-zero highs were recorded in Montana, Wyoming and Colorado, and sub-freezing highs were recorded as far as Texas. [14]
On November 13, Casper, Wyoming had its lowest temperature ever recorded in November, with a record low of −27 °F (−33 °C), and Denver, Colorado had a low of −14 °F (−26 °C), the second-coldest ever recorded for that month. [14] On November 18, Detroit tied a record of 11 °F (−12 °C), first set in 1880. [15] Cleveland also tied a record low that morning of 10 °F (−12 °C), first set in 1959, and also became the coldest temperature for any date so early in the season in Cleveland since 1959 as well. [16] Jacksonville, Florida reached 24 °F (−4 °C) on November 20, 2014, breaking a record set in 1873. [17]
The cold wave brought an end to the navigation season on the upper Mississippi River, the earliest closing since records began in 1969. [18]
Overall, November 2014 was the 16th coldest November in the contiguous United States, and the coldest since 2000. Alabama and Mississippi saw their 2nd coldest November, and 16 other states had a top ten cold November. [19]
A severe and persistent lake-effect snow event hit the Great Lakes snowbelt regions, triggered by a winter storm that emerged from Canada, to the north of the Midwest.
On November 10, St. Cloud, Minnesota had the biggest snowfall ever in November with 13.2 inches (34 cm). By the next day, Ishpeming, Michigan had 24.5 inches (62 cm), the most of any location. [20]
In Buffalo, New York, another winter storm triggered a strong lake-effect band, which impacted the city and its immediate southern suburbs from November 17–19, 2014, with a second wave hitting November 20 before shifting southward and weakening. [21] As much as 65 inches fell in Cheektowaga. Snow fell at rates as high as five inches per hour. [22] However, nearby regions of Buffalo only received between one and six inches from the storm. [23] Once the band dissipated, the risk of flooding became a significant concern, as temperatures were forecast to rise sharply and rain was forecast to enter the area beginning November 23, causing the snowpack to melt rapidly. [24]
South Bend, Indiana received 12.3 inches on November 13, breaking its old record for that day of five inches. [25]
Snow depths of greater than 24 inches were reported in numerous location across the Upper Peninsula of Michigan. [26] with 42.5 inches reported near Ishpeming between November 10–12. [27] Gaylord and Sault Ste. Marie, Michigan had each reported over 50 inches of snow in November. [28] Allendale in west Michigan received 20.4 inches with 17 inches in East Grand Rapids. [29]
On November 23, the formation of a ridge of high pressure across the Southeastern United States forced the polar vortex fragment over the Eastern United States to retreat back to Canada, allowing a warming trend across much of the Midwest and the Eastern United States. [1] However, this same warming trend brought concerns that the resulting snowmelt and incoming rain may cause floods in the region. [1] [5]
Sustained winds of 110 km/h (70 mph) with gusts to 156 km/h (97 mph) were recorded on the island of Shemya. [30] Only minor damage was reported on the island which houses a United States Air Force installation. [31] On November 12, a winter storm in the Great Lakes region killed four people in Minnesota. [3] On November 17, another winter storm caused the deaths of at least 11 people in traffic-related accidents. [4] By November 19, another seven people had died in western New York from the cold temperatures brought by that same winter storm. [32] On November 20, another person died from the cold. [33] On November 22, the death toll from the November 13–21 winter storm increased to 13 fatalities (not including 11 earlier traffic accidents). [5] In addition, early on November 20, a man froze to death near Chicago. The temperature was 14 °F (−10 °C). [34]
The Great Blizzard of 1899, also known as the Great Arctic Outbreak of 1899 and the St. Valentine's Day Blizzard, was an exceptionally severe winter weather event that affected most of the United States, particularly east of the Rocky Mountains. On February 11, Swift Current in present-day Saskatchewan reported a record-high barometric pressure of 31.42 inches of mercury (1,064 mb). While there was heavy snow during this event, the 1899 storm was most noted for the record cold it brought to several areas of the USA, including the first below 0 °F (−17.8 °C) temperature ever recorded in Florida, when the state capital Tallahassee in the extreme northern Panhandle recorded −2 °F or −18.9 °C.
A cold wave is a weather phenomenon that is distinguished by a cooling of the air. Specifically, as used by the U.S. National Weather Service, a cold wave is a rapid fall in temperature within a 24-hour period requiring substantially increased protection to agriculture, industry, commerce, and social activities. The precise criteria for a cold wave are the rate at which the temperature falls, and the minimum to which it falls. This minimum temperature is dependent on the geographical region and time of year.
North Dakota's climate is typical of a continental climate with cold winters and warm-hot summers. The state's location in the Upper Midwest allows it to experience some of the widest variety of weather in the United States, and each of the four seasons has its own distinct characteristics. The eastern half of the state has a humid continental climate with warm to hot, somewhat humid summers and cold, windy winters, while the western half has a semi-arid climate with less precipitation and less humidity but similar temperature profiles. The areas east of the Missouri River get slightly colder winters, while those west of the stream get higher summer daytime temperatures. In general, the diurnal temperature difference is prone to be more significant in the west due to higher elevation and less humidity.
The 1994 North American cold wave occurred over the midwestern and eastern regions of the United States and southern Canada in January 1994. The cold wave caused over 100 deaths in the United States. Two notable cold air events took place from January 18–19 and January 21–22. There were 67 minimum temperature records set on January 19. During this time, much of the United States experienced its coldest temperatures since a major storm on February 20, 1934.
The January–March 2014 North American cold wave was an extreme weather event that extended through the late winter months of the 2013–2014 winter season, and was also part of an unusually cold winter affecting parts of Canada and parts of the north-central and northeastern United States. The event occurred in early 2014 and was caused by a southward shift of the North Polar Vortex. Record-low temperatures also extended well into March.
The 2013–14 North American winter was one of the most significant for the United States, due in part to the breakdown of the polar vortex in November 2013, which allowed very cold air to travel down into the United States, leading to an extended period of very cold temperatures. The pattern continued mostly uninterrupted throughout the winter and numerous significant winter storms affected the Eastern United States, with the most notable one being a powerful winter storm that dumped ice and snow in the Southeastern United States and the Northeastern United States in mid-February. Most of the cold weather abated by the end of March, though a few winter storms did affect the Western United States towards the end of the winter.
The November 2014 Bering Sea cyclone was the most intense extratropical cyclone ever recorded in the Bering Sea, which formed from a new storm developing out of the low-level circulation that separated from Typhoon Nuri, which soon absorbed the latter. The cyclone brought gale-force winds to the western Aleutian Islands and produced even higher gusts in other locations, including a 97 miles per hour (156 km/h) gust in Shemya, Alaska. The storm coincidentally occurred three years after another historic extratropical cyclone impacted an area slightly further to the east.
The 2014–15 North American winter was frigid and prolifically wintry, especially across the eastern half of North America in the months of January–March. The season began early, with many places in North America experiencing their first wintry weather during mid-November. A period of below-average temperatures affected much of the contiguous United States, and several records were broken. An early trace of snowfall was recorded in Arkansas. There were greater accumulations of snow across parts of Oklahoma as well. A quasi-permanent phenomenon referred to as the polar vortex may have been partly responsible for the cold weather. Temperatures in much of the United States dropped 15 to 35 °F below average by November 19, following a southward "dip" of the polar vortex into the eastern two-thirds of the country. The effects of this dip were widespread, bringing about temperatures as low as 28 °F (−2 °C) in Pensacola, Florida. Following a significant snowstorm there, Buffalo, New York received several feet of snow from November 17–21. In addition, significant winter weather occurred throughout the season, including a major blizzard that struck the Northeastern United States at the end of January, another blizzard that affected much of the Northern United States days later in early February, and several significant snow events paired with very frigid temperatures for much of February.
The 2015–16 North American winter was not as frigid across North America and the United States as compared to the 2013–14 and 2014–15 winters. This was mainly due to a strong El Niño, which caused generally warmer-than-average conditions. However, despite the warmth, significant weather systems still occurred, including a snowstorm and flash flooding in Texas at the end of December and a large tornado outbreak at the end of February. The main event of the winter season, by far and large, was when a crippling and historic blizzard struck the Northeastern United States in late January, dumping up to 3 feet of snow in and around the metropolitan areas. Several other smaller snow events affected the Northeast as well, but for the most part the heaviest snowstorms and ice stayed out further west, such as a severe blizzard in western Texas in late December, and a major late-season snowstorm in Colorado in mid-April.
The January 2–4, 2014 North American blizzard was a major winter storm that affected much of the East Coast with snow, and frigid temperatures following the storm. The storm had dumped up to 2 ft (0.61 m) of snow in some areas, especially around Boston, Massachusetts.
The February 2015 North American cold wave was an extreme weather event that affected most of Canada and the eastern half of the United States. Following an earlier cold wave in the winter, the period of below-average temperatures contributed to an already unusually cold winter for the Eastern U.S. Several places broke their records for their coldest February on record, while some areas came very close. The cause of the cold wave was due to the polar vortex advancing southward into the eastern parts of the U.S, and even making it as far south as the Southeast, where large snow falls are rare. By the beginning of March, although the pattern did continue for the first week, it abated and retreated near the official end of the winter.
The 2017–18 North American winter saw weather patterns across North America that were very active, erratic, and protracted, especially near the end of the season, resulting in widespread snow and cold across the continent during the winter. Significant events included rare snowfall in the South, an outbreak of frigid temperatures that affected the United States during the final week of 2017 and early weeks of January, and a series of strong nor'easters that affected the Northeastern United States during the month of March. In addition, flooding also took place during the month of February in the Central United States. Finally the winter came to a conclusion with a powerful storm system that caused a tornado outbreak and blizzard in mid-April. The most intense event, however, was an extremely powerful cyclonic blizzard that impacted the Northeastern United States in the first week of 2018. Similar to the previous winter, a La Niña was expected to influence the winter weather across North America.
The December 2017–January 2018 North American cold wave was an extreme weather event in North America in which record low temperatures gripped much of the Central, Eastern United States, and parts of Central and Eastern Canada. Starting in late December as a result of the southward shift of the polar vortex, extremely cold conditions froze the eastern United States in the last few days of 2017 as well as into the new year. Following a brief respite in mid-January, cold temperatures swung back into the eastern U.S. shortly afterwards. The cold wave finally dissolved by around January 19, as near-average temperatures returned.
The 2018–19 North American winter was unusually cold within the Northern United States, with frigid temperatures being recorded within the middle of the season. Several notable events occurred, such as a rare snow in the Southeast in December, a strong cold wave and several major winter storms in the Midwest, and upper Northeast and much of Canada in late January and early February, record snowstorms in the Southwest in late February, deadly tornado outbreaks in the Southeast and a historic mid-April blizzard in the Midwest, but the most notable event of the winter was a record-breaking bomb cyclone that affected much of the Central United States and Canada in mid-March. Unlike previous winters, a developing weak El Niño was expected to influence weather patterns across North America. Overall, however, winter of 2018–19 had many La Niña like conditions, being mild along the mid- and lower parts of the East Coast, the West Coast, and most of the southern Plains. Overall, the meteorological winter of 2018-19 became the wettest on record for the United States.
In late January 2019, a severe cold wave caused by a weakened jet stream around the Arctic polar vortex hit the Midwestern United States and Eastern Canada, killing at least 22 people. It came after a winter storm brought up to 13 inches (33 cm) of snow in some regions from January 27–29, and brought the coldest temperatures in over 20 years to most locations in the affected region, including some all-time record lows. In early February, a concentration of Arctic air colloquially referred to as the "polar vortex" moved west, and became locked over Western Canada and the Western United States. As a result, February 2019 was among the coldest and snowiest on record in these regions. In early March, the cold once again shifted east, breaking records in many areas. In mid-March, the cold wave finally retreated, but combined with above-average temperatures, precipitation, and a deep snowpack, widespread flooding ensued in the Central US.
The 2019–20 North American winter was unusually warm for many parts of the United States; in many areas, neutral ENSO conditions controlled the weather patterns, resulting in strong El Niño like conditions and the sixth-warmest winter on record, and many areas in the Northeastern United States saw one of the least snowy winters in years. In fact, Baltimore and Islip saw no snow in February for the first time. Some notable events still occurred, such as a powerful blizzard that impacted the Western United States in late November, a series of cold shots in January and February, a snowstorm within the Texas Panhandle and a late-season blizzard in the High Plains.
The 2020–21 North American winter was the most significant winter season to affect North America in several years, and the costliest on record, with a damage total of at least $33.35 billion. The season featured six storms ranking on the Regional Snowfall Index scale (RSI), with four storms ranking as at least a Category 3. Most of the winter's damage and fatalities occurred due to a historic and major cold wave in mid-February. Several other significant events occurred, including a crippling early-season ice storm in the Southern Plains, a powerful nor'easter in mid-December, another major nor'easter in early February, two major and widespread winter storms in mid-February, and a major blizzard in the Rocky Mountains in mid-March. The winter-related events were responsible for at least 358 fatalities, making it the deadliest season since 1992–93. A La Niña pattern influenced much of the winter in North America.
The February 2021 North American cold wave was an extreme weather event that brought record low temperatures to a significant portion of Canada, the United States and parts of northern Mexico during the first two-thirds of February 2021. The cold was caused by a southern migration of the polar vortex, likely caused by a sudden stratospheric warming event that occurred the prior month. Temperatures fell as much as 25–50 °F below average as far south as the Gulf Coast. Severe winter storms also were associated with the bitter cold, which allowed for heavy snowfall and ice accumulations to places as far south as Houston, Texas, and contributing to one of the snowiest winters ever in some areas in the Deep South.
The 2022–23 North American winter was an unusually warm winter for the east and an unusually cold winter for the west in North America, as it occurred across the continent from late 2022 to early 2023. The winter season in North America began at the winter solstice, which occurred on December 21, 2022, and it ended at the March equinox, which occurred on March 20, 2023. The first day of meteorological winter began on December 1 and unofficially ended on February 28; winter storms may still occur outside of these limits.
From December 21 to 26, 2022, an extratropical cyclone created crippling winter storm conditions, including blizzards, high winds, snowfall, and record cold temperatures across the majority of the United States and parts of Canada. Areas which experienced blizzard conditions included parts of Minnesota, Iowa, Wisconsin, Michigan, Ohio, Pennsylvania, New York and Ontario, with the Buffalo area of New York and the Fort Erie and Kingston areas of Ontario experiencing almost two full days of blizzard/zero-visibility conditions starting from December 23. The cold wave affected all U.S. states from Colorado to the Eastern Seaboard, with effects felt as far south as Miami, Florida. On December 24, 110 million people across 36 states were subject to wind chill alerts.
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