2013–14 North American winter
|2013–14 North American winter|
A temperature map of the frigid conditions in the United States on January 2–4, 2014
|Astronomical winter||December 21 – March 20|
|Meteorological winter||December 1 – February 28|
|Most notable event|
|Name||Mid-February 2014 North American winter storm|
|Duration||February 11–24, 2014|
|Maximum snow accumulation|
|Highest snowfall total||58 in (150 cm) (Lead, South Dakota)|
|Event||October 3–7, 2013|
The 2013–14 North American winter refers to winter in North America as it occurred across the continent from late 2013 through early 2014. While there is no well-agreed-upon date used to indicate the start of winter in the Northern Hemisphere, there are two definitions of winter which may be used. Based on the astronomical definition, winter begins at the winter solstice, which in 2013 occurred on December 21, and ends at the March equinox, which in 2014 occurred on March 20. Based on the meteorological definition, the first day of winter is December 1 and the last day February 28. Both definitions involve a period of approximately three months, with some variability.
- 1 Seasonal forecasts
- 2 Events
- 2.1 October storm complex
- 2.2 Late November storm complex
- 2.3 December cold wave
- 2.4 Early December winter storm
- 2.5 Pre-Christmas storm complex
- 2.6 Early 2014 cold wave and nor'easter
- 2.7 Late January blizzard
- 2.8 Late January winter storm
- 2.9 Mid-February winter storm
- 2.10 Late February storm complex
- 2.11 Early March winter storm
- 2.12 March ice storm
- 2.13 Late March bomb cyclone
- 2.14 Early April storm complex
- 3 See also
- 4 References
- 5 External links
On November 21, 2013, the National Oceanic and Atmospheric Administration's Climate Prediction Center issued its U.S. Winter Outlook. Sea surface temperatures had been near average since spring 2012, and forecasters expected these conditions to continue through winter 2013–14, with neither El Niño nor La Niña conditions expected to affect the season's climate. In the outlook, little rainfall was anticipated in the Southwestern United States, and the development of drought was expected in the Southeastern United States. Below-average levels of precipitation and below-average temperatures were expected in the Alaskan panhandle. Below-average temperatures were also favored in the Northern Plains, while above-average temperatures were favored in New England, the South-Central, Southeastern, and Southwestern United States, and western Alaska. The remainder of the country fell into the outlook's "equal chance" category, with an equal chance of above-average, below-average, and near-average temperatures and/or precipitation.
October storm complex
The first winter storm of the season, a significant system, was forecast by the National Weather Service, which issued a Blizzard Warning on October 3 preceding the storm. The storm occurred as an early season blizzard, and, according to the Weather Prediction Center, was an event of a magnitude unseen for the past decade. Many locations in Colorado, Nebraska, Montana, Wyoming, , and received near or over 10 inches (25 cm) of snow. Some areas in South Dakota received nearly 4 feet (1.2 m) of snow, with receiving 47 inches (120 cm). In many locations, there were high winds of over 50 miles per hour (80 km/h), with some locations reporting winds of nearly hurricane force, being 74 miles per hour (119 km/h).
Late November storm complex
The Weather Channel meteorologist Jonathan Erdman described the storm as "about as expansive a winter storm as it get," On November 24, 2013, 300 flights were cancelled at Dallas-Fort Worth International Airport. Flagstaff, Arizona recorded 11 inches of snow, and near the Four Corners as much as 4 feet fell. As much as a foot of snow fell in Colorado and Utah, and 13 people had died as of November 25. The serious winter storm that was expected did not materialize. As of November 27, 2013, 475 flights had been cancelled, with 3,600 delays, many in the New York City and Philadelphia areas. Snow turned to rain in Pittsburgh despite an ominous forecast, but 9 inches fell in Mercer County, Pennsylvania and 4.5 inches in Buffalo. Atlanta had less than an inch of snow, but it was the third November snow since 1930. Morehead City, North Carolina had serious damage, and damage was also reported in Atlantic Beach, North Carolina, from an EF2 tornado.
December cold wave
On December 1, 2013, the weakening of the polar vortex led to the beginning of an abnormally cold trend in the Eastern and Central United States. On December 6, the continued deterioration of the polar vortex led to the jet stream pushing southward, bringing record cold temperatures across the Eastern U.S. During the cold wave, which extended from December 6–10, over 150 daily precipitation records and close to 100 daily snowfall records were broken across the northeastern, southeastern and south central United States. Numerous airline flights were canceled and there were reports of power outages.
Early December winter storm
On December 2, a Pacific storm system entered the Western United States, and it spread heavy rain and snow from the Pacific coast to the Rocky Mountains. As the storm continued to move east, high snow totals fell in its wake. Maximum reported snowfall totals in this area were found to have occurred in Idaho, Wyoming, and Montana, where 30 inches (76 cm) or greater were reported. High winds were widespread as well, with multiple locations in the mountainous regions of the western US reporting winds of greater than 60 miles per hour (97 km/h). As reported by the National Weather Service's Weather Prediction Center, the surface low reached its peak strength at approximately 6:00 UTC on December 3 while it was over western Wyoming, where a central pressure of 994 hectopascals (994 mbar; 29.4 inHg) was observed.
Pre-Christmas storm complex
On December 19, a strong cold front moved southward across much of the Great Plains. By daybreak on December 20, temperatures in many parts of Oklahoma had dropped to mostly between 10 and 30 °F (−12 and −1 °C). However, despite the freezing temperatures, the depth of the cold air was rather shallow, with a depth of generally no more than 1,500 feet (460 m). As a result of the shallow depth of the front, once the front reached parts of the higher terrain in northwestern Arkansas, the front stalled, leaving areas just ahead of the front significantly colder than areas behind it. While temperatures in much of the Plains remained at or below freezing, an upper low was forming over the Southwestern United States. As the low pushed eastward and northeastward across parts of eastern New Mexico and West Texas, it interacted with moisture over the Southern Plains; there was an unusually high amount of moisture across the area for December, and the low drew much of it over the cold air-mass near the surface. With the moisture in place, light rain began to fall in some locations prior to sunset. The rain persisted and spread from southwest to northeast overnight, with moderate rain beginning to fall across much of Southwest, Central, and northeastern Oklahoma and Southeast Kansas. By late morning on December 21, much of the rain had ended in Southwest and Central Oklahoma, where many areas had received over 0.25 inches (0.64 cm) of ice accumulation with some locations receiving over 0.50 inches (1.3 cm) or even, in localized areas, 0.75 inches (1.9 cm) of ice; isolated power outages occurred, and multiple trees and tree limbs were broken and/or pulled down by the weight of the ice. Heavy icing continued along the Interstate 44 corridor and parts of Osage County in Oklahoma; in these areas, there were reports of 0.50–0.75 inches (1.3–1.9 cm) of ice, and in southeastern Oklahoma and extreme northwestern Arkansas, there were lesser reports of 0.25–0.50 inches (0.64–1.27 cm) of ice. Additional ice totals occurred in Southeast Kansas, where there were isolated locations which received ice accumulations of as high as 0.75 inches (1.9 cm).
Early 2014 cold wave and nor'easter
2014 began on an active note, with a major winter storm affecting much of the United States. Between 6 and 12 inches (150 and 300 mm) of snow fell across a wide area spreading from central Missouri across Illinois and Indiana to Lower Michigan. Snowfall totals of near 18 inches (460 mm) were recorded across northern Indiana, and additional accumulations occurred downwind from the major Great Lakes. This storm was accompanied by some of the coldest temperatures to affect the Central and Eastern United States in 20 years. Upper flow which was meridional all the way up to the Arctic Circle provided a direct path for cold air advection to occur southward to the United States. The average temperature of the contiguous United States was 17.9 °F (−7.8 °C), the coldest day since January 12–13, 1997 and the 40th-coldest day in the United States since 1900. During the event, wind chills dropped as low as the -60s °F (-50s °C) across the Northern High Plains. The event was short-lived, with the portion of the polar vortex that had traveled across the Great Lakes lifting northeastward into Quebec soon after.
Late January blizzard
On January 20, a moisture-starved Alberta clipper zipped through the Upper Midwest, putting down anywhere from 1–3 inches (2.5–7.6 cm). As it moved towards the East Coast, it began to intensify and snowfall began to spread from areas like Washington D.C to Hartford, Connecticut. A surface low formed and began to track northwards, with winds increasing along the coastline, causing blizzard conditions. It then continued to rapidly intensify before reaching a peak of 962 millibars (28.4 inHg). Snowfall totals from this storm ranged anywhere from 12–18 inches (30–46 cm). The storm was also proceeded by more cold temperatures as well.
Late January winter storm
Early on January 27, a cold front crossed into the Gulf of Mexico, with temperatures ahead of the front in Texas and Louisiana in the 60s °F (10s °C) dropping to below freezing only one day later. As this occurred, a southern stream upper-level trough translated in an eastward direction across northern parts of Mexico. This also coincided with the backing of low-level winds along the western Gulf Coast. Relatively warm and humid air overrode the colder air near the surface, resulting in precipitation falling in Texas, Louisiana, and parts of the Southeastern U.S. as a mixture of rain, freezing rain, and snow. Late in the day, a broad northern stream upper-level trough containing a trough axis was located over the Central and Eastern United States, and the storm began to develop as this trough axis, initially reaching from the Upper Midwest to the northern Rocky Mountains, sharpened and moved in a southeastward direction during the following 24-hour period. This activity coincided with the movement of additional cold air at the surface. Many areas experiencing liquid precipitation falling at the surface saw rain switch over to freezing rain by 12:00 UTC January 28 as temperatures dropped. A mixture of frozen to partly frozen precipitation spread eastward over the following period into the early hours of January 29, impacting much of the Deep South. Widespread ice accumulations in excess of .25 inches (6.4 mm) occurred as a result of the event. As the southern stream trough axis weakened while it moved eastward across the western Gulf of Mexico, a northern stream trough amplified as it headed toward the Southeastern U.S. Overrunning wintry precipitation affected the area as a weak surface low traveled along the front and crossed into the Atlantic.
Mid-February winter storm
On February 11, a quick-moving area of low pressure moved across the Southeast, bringing rain and snow to areas like Atlanta, interacting with some of the cold air to the north of it. It then quickly moved offshore by roughly 3 p.m. This part of the storm was only the beginning of a crippling 2-day streak of winter nightmares across the South. Accumulations from this half of the winter storm ranged anywhere from 1–3 inches (2.5–7.6 cm) of snow and a glaze of icing across the South.
Later on February 11, another area of low pressure formed on the extreme southern edge of the Gulf Coast, near the TX–LA border. Drawing moisture from the Gulf of Mexico, it was able to fire up a small area of showers and thunderstorms near the coastline. As it tracked eastward, it began to interact with the cold air above it, producing an area of ice and snow on its backside as it moved to the east. On February 12, the swath of ice exploded in size as the conditions for freezing rain began to come together. Areas from eastern Alabama, including Atlanta in Georgia to the Southeast coast and South Carolina were included in this swath of icy precipitation. Meanwhile, to the south, near the Gulf Coast, heavy showers and thunderstorms were consisted in a streak of rain stretching up to southern parts of Georgia. As the low moved east, it then dissipated as a new area of low pressure developed off the South Carolina coast late on February 12, and that began to strengthen as it tracked to the north, placing the Northeast in the fire zone for the winter storm.
Early on February 13, more snow began to develop on the northern side of the storm as the precipitation shield approached the Tri-State Area in colder air. Heavy bands of snow set up as the system began its transition into a nor'easter, with some of these bands containing snowfall rates of up to 1–2 inches (2.5–5.1 cm) per hour. At the same time, warmer air was beginning to funnel into the storm system, and as a result the rain/snow line slowly creeped up the state of New Jersey as the warm air began to further intrude into the winter storm. By 10 a.m, most of the precipitation had moved north of New York City, and began to reach into areas like Boston. Even though the area of low pressure, which had now deepened to 988 millibars (29.2 inHg) late on February 13, was offshore of the East Coast, little to no precipitation was falling as a result of dry air to funnel its way into the storm. Most of the snow totals in these areas ranged anywhere from 6–24 inches (0.50–2.00 ft), as a result.
Late February storm complex
On February 19, an area of low pressure moved out the High Plains into the Midwest. Originally devoid of moisture, it began to track to the north. Drawing moisture from the Gulf of Mexico, it began to intensify. This was thrown back into cold air that was situated over parts of the Midwest at the time. As a result, an intense swath of snow developed from northern parts of Nebraska to western Iowa near Omaha early on February 20. As the storm system continued to move northwards, the winds began to pick up, setting the stage for blizzard conditions. Thundersnow was also observed in parts of the affected areas, due to the instability in the atmosphere. Wind gusts of up to 60 mph (97 km/h) and 12–24 inches (30–61 cm) of snow were reported from this system.
Another threat from this system was the potential of severe weather. As the winter storm moved to the north, a long squall line of heavy showers and thunderstorms fired up ahead of its cold front. Most of the main threats from this portion of the system was damaging winds and hail, with the isolated chance of a tornado. The squall line rapidly weakened as it progressed towards the East Coast.
The massive system continued to produce hefty snowfall and strong winds even after it weakened on February 21; it was slowly retreating into Canada. It finally dissipated on February 22.
Early March winter storm
On February 28, an extratropical cyclone moved near California. Showers and thunderstorms began spreading into California early on March 1 which is the atmospheric river with heavy snowfall in the mountains, torrential rainfall, triggering numerous flash floods, and even spawning two EF0 tornadoes in Arizona and California The storm weakened somewhat as it began to pass through the southwestern United States, but maintained its structure as it began to move towards the central part of the country.
At the same time, an Alberta clipper was moving through the Upper Midwest, dropping relatively light to moderate snow through the areas. The energy between the clipper system and the remains of the extratropical cyclone combined to produce energy for a long tracked winter storm. Late on March 2, snow and ice began to develop along a weak area of low pressure near Texas. A small squall line began to set up ahead of the cold front, although there wasn't any tornadoes produced by the system. Snow and ice began to reach into the Mid-Atlantic near midnight, which eventually started to sag southwards, keeping most of the heaviest snow accumulations to the south of the Northeast. The system then moved off by evening on March 3. Snowfall accumulations ranged from 3–7 inches (7.6–17.8 cm) from the winter storm. At least 16 fatalities were reported.
March ice storm
A gulf low moved inland over the peninsula of Florida on March 5, bringing abundant moisture into the Southeast. An area of high pressure settled in over the Northeast, which pushed cold air down into the Southeast. This set the stage for an ice storm in those areas. On March 6, the northern edge of the system moved into the cold air, and ice began to break out in northern parts of the Carolinas. Ice accumulations totaled up to 1 inch (25 mm) in some of the hardest hit areas, which some did not have power for several days. On the colder side of the ice storm, snow accumulations ranged up to 16 inches (41 cm) in the higher elevations. The system then turned to the east and moved offshore near the North Carolina–South Carolina border late on March 7 and accelerated into the northern Atlantic Ocean.
Late March bomb cyclone
Late on March 25, a winter storm emerged off the coast of the Southeastern United States and began to undergo explosive intensification, becoming a meteorological bomb by March 26. Powered by moisture coming from the Gulf of Mexico, the storm quickly became an unusually powerful nor'easter four times the size of , and reached a maximum low pressure of 954 mbar (28.2 inHg; 95.4 kPa). The system produced powerful sustained winds up to 89 mph (143 km/h), and wind gusts up to 119 mph (192 km/h), with unofficial amounts reaching 129 mph (208 km/h). After making landfall on Nova Scotia, the system weakened to a 960 mbar (28 inHg; 96 kPa) nor'easter on March 27, before weakening further to a 975 mbar (28.8 inHg; 97.5 kPa) storm on March 28. On March 29, the system deteriorated into a weak winter storm over Greenland, where it would remain for the next few days while slowly dissipating.
Early April storm complex
At the beginning of April, a rare snow event set up in the Midwest, something uncommon in those areas. On April 2, an area of low pressure was over California, and began to move eastward. Following this, it began to turn to the northeast, setting its target on the upper Midwest, which was already above snowfall for the season. Wet snowfall began to fall near Denver allowing 2–6 inches (5.1–15.2 cm) to accumulate. The system then began spread snowfall on a northeast axis, and it began to move into parts of Minnesota and Wisconsin, at the same time, severe thunderstorms started firing up along the cold front, which also contributed to a tornado outbreak.
Meanwhile, the storm continued to crank out snowfall as it began to accelerate somewhat, drawing cold air into parts of the upper Midwest, where it began to produce more snowfall where rates approached 2 inches per hour. The storm complex moved into Canada. Snowfall totals from this late-season winter storm reached as high as 18 inches (46 cm) (with a sharp snowfall gradient near Minneapolis), however it melted rapidly soon afterwards due to warm temperatures filtering in the days after the storm.
- Global storm activity of 2010
- Early 2014 North American cold wave
- November 2014 North American cold wave
- Cold wave
- Polar vortex
- Winter storm
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- 2013 Storm Summaries from the Weather Prediction Center
- 2014 Storm Summaries from the Weather Prediction Center
- Major Winter Weather Events during the 2013-2014 Cold Season (WPC)
| North American winters