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January 2000 North American blizzard

Winter storm in North America From Wikipedia, the free encyclopedia

The Carolina Crusher was one of the most powerful winter storms on record in parts of North Carolina, USA. The storm impacted the Greater Richmond Region on January 25th, 2000, causing thousands of power outages and leaving 11 in (280 mm) of snow in Richmond, Virginia, and 20.3 in (520 mm) at Raleigh-Durham International Airport before moving out into the Atlantic Ocean.

FormedJanuary 18, 2000
DissipatedJanuary 30, 2000
Max.snowfall20–30 in (51–76 cm) – Raleigh-Durham
Damage$800 million in North Carolina[1]
Quick facts Meteorological history, Formed ...
The Carolina Crusher
Meteorological history
FormedJanuary 18, 2000
DissipatedJanuary 30, 2000
Category 3 "Major" blizzard
Regional snowfall index: 7.86 (NOAA)
Max. snowfall20–30 in (51–76 cm) – Raleigh-Durham
Overall effects
Damage$800 million in North Carolina[1]
Areas affectedEastern United States, Eastern Canada
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Meteorological history

The storm began forming during a mild winter with below-average snowfall across much of the East Coast. Snow first started falling on Wednesday, January 19th, the major storm portion began on Friday, January 21st, 2000.

Initially, computer models suggested that an area of low-pressure would develop and, after getting energy from another low-pressure system in Canada, track up the East Coast. But over the weekend, some computer models no longer showed a strong storm. By Monday, January 24th, forecasters called only for "snow flurries" and "up to an inch of accumulation on the ground."[3]

Some meteorologists considered classifying the event as part of the Big Storm which was occurring in Canada at the time. The North American storm's low-pressure system originated over the northern Great Lakes, then entered over Appalachia where it strengthened considerably. Following this, it went into the North again to collide with the warm front that was approaching.

Progression of the storm

A dip in the jet stream had created a trough, which caused rain in northern Florida and snow in Georgia. By the morning of the 24th, the storm was located in the northeastern Gulf of Mexico near Apalachicola, Florida. By the evening of the 24th, it was rapidly intensifying against the South Carolina coast. By Tuesday, January 25th, it was near Hatteras, North Carolina. The storm moved northeastward along the Atlantic Seaboard. Later in the day, it was located 80 miles east of Long Beach Island, New Jersey. It then began to weaken and by the morning of the 26th, it was located just east of Portland, Maine. The storm was poorly forecast because of other simultaneous storm events and the awkward buildup of two low-pressure systems.[2]

Impact of the storm

Progress throughout the northern territories, including Pennsylvania, Delaware, and New Jersey, was significantly more damaging due to high winds, wet snow, sleet, and freezing rain. Snowfall rates of around 2 inches per hour were common during the first hours of this storm. Businesses, schools, airports, malls, and government offices were closed on January 25th due to weather.

In Pennsylvania, this was the most significant winter storm since the Blizzard of 1996. Most municipalities declared the standard snow emergencies where accidents, traffic hazards, and power outages occur. About 2,000 homes and businesses lost power, mainly in the Philadelphia area.

For Delaware, the change from wet snow to heavy, dry snow helped cut down on the amount of damage.

In addition to heavy snow, New Jersey also experienced wind gusts as strong as 60 mph along the shore, moderate coastal flooding, and drifts as high as 4 feet. The storm's intensity was lighter during the late morning and afternoon hours before strengthening again in the evening. The winter storm caused numerous accidents around the region.

In the southwestern territories, the wind was not as severe as in the north. In Richmond, Virginia, the snow fell as sleet then immediately turned into dry snow. The power outages came late the following week due to the rise in temperatures, with the snow already on the ground becoming wet snow.[3]

Charlotte, North Carolina received almost a foot of snow in a 12 hour period. Raleigh, North Carolina and Annapolis, Maryland both had 20-24 inches, while Washington, D.C. had 14 inches. Areas that had less snowfall include Boston, Massachusetts and New York City, New York which both had 5 inches.[4]

Loss and damages

Raleigh and other areas of North Carolina were shut down for many days due to large amounts of snow remaining and poor road conditions.

There were at least three confirmed deaths from heart attacks shoveling snow in Pennsylvania. In Maryland, the National Weather Service reported at least eight deaths.[5]

Total accumulations

Pennsylvania and Delaware

More information County, Location ...
County Location Amount
Monroe County Saylorsburg 13 in (33 cm)
Long Pond 11 in (28 cm)
Bossardsville 10 in (25 cm)
East Stroudsburg 10 in (25 cm)
Scotia 7 in (18 cm)
Pocono Summit 6.5 in (17 cm)
Northampton County Williams Township 14 in (36 cm)
Bath 7 in (18 cm)
Lehigh County Allentown 7 in (18 cm)
Lehigh Valley Airport 10 in (25 cm)
Berks County Blue Marsh Lake 11 in (28 cm)
Morgantown 10 in (25 cm)
Vinemont 10 in (25 cm)
Kutztown 8 in (20 cm)
Lincoln Park 8 in (20 cm)
Chester County Kennett Square 12 in (30 cm)
West Barlborough Township 12 in (30 cm)
Downingtown 11 in (28 cm)
West Chester 11 in (28 cm)
Coatesville 9 in (23 cm)
Honey Brook 8 in (20 cm)
Glenmoore 8 in (20 cm)
Montgomery County Willow Grove 14 in (36 cm)
Wynnewood 12 in (30 cm)
Norristown 11.5 in (29 cm)
King Prussia 11 in (28 cm)
Pottstown 7 in (18 cm)
Bucks County Chalfont 13.6 in (35 cm)
Furlong 12.5 in (32 cm)
Doylestown 12 in (30 cm)
Springtown 9 in (23 cm)
Langhorne 9 in (23 cm)
Delaware County Springfield 11 in (28 cm)
Philadelphia International Airport 9 in (23 cm)
New Castle County New Castle County Airport 10 in (25 cm)
Kent County Woodside 11 in (28 cm)
Dover 11 in (28 cm)
Milford 9 in (23 cm)
Viola 8 in (20 cm)
Sussex County Georgetown 8.5 in (22 cm)
Seaford 8 in (20 cm)
Lewes 6.5 in (17 cm)
Laurel 6 in (15 cm)
Rehoboth Beach 5 in (13 cm)
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New Jersey

More information County, Location ...
County Location Amount
Sussex County High Point 15 in (38 cm)
Culver Lake 14.7 in (37 cm)
Wantage 13.5 in (34 cm)
Sparta 9.5 in (24 cm)
Sussex 8 in (20 cm)
Warren County Phillipsburg 12 in (30 cm)
Allamuchy 11 in (28 cm)
Morris County Oak Ridge 12 in (30 cm)
Long Valley 11 in (28 cm)
Whippany 9 in (23 cm)
Rockaway 9 in (23 cm)
Madison 6 in (15 cm)
Hunterdon County White House Station 13 in (33 cm)
Califon 11.5 in (29 cm)
Flemington 10 in (25 cm)
Wertsville 10 in (25 cm)
Somerset County Neshanic 10.5 in (27 cm)
Pottersville 10 in (25 cm)
Branchburg 9 in (23 cm)
Somerville 9 in (23 cm)
Middlesex County New Brunswick 6 in (15 cm)
Woodbridge 6 in (15 cm)
Mormouth County Ocean Grove 7 in (18 cm)
Manasquan 7 in (18 cm)
Howell 6 in (15 cm)
Union Beach 6 in (15 cm)
Mercer County Washington's Crossing 10 in (25 cm)
Princeton 8 in (20 cm)
Hightstown 8 in (20 cm)
Burlington County Moorestown 13 in (33 cm)
Lumberton 10 in (25 cm)
Marlton 10 in (25 cm)
Mount Laurel 9 in (23 cm)
Bordentown 7 in (18 cm)
Ocean County Brick 10 in (25 cm)
Brant Beach 9 in (23 cm)
Jackson 8 in (20 cm)
Camden County Gloucester City 13 in (33 cm)
Somerdale 11 in (28 cm)
Pennsauken 10 in (25 cm)
Cherry Hill 8 in (20 cm)
Gloucester County Sewell 13 in (33 cm)
Mullica Hill 13 in (33 cm)
Swedesboro 11.5 in (29 cm)
Salem County Deepwater 10.3 in (26 cm)
Cumberland County Seabrook 9 in (23 cm)
Millville 8 in (20 cm)
Vineland 7 in (18 cm)
Atlantic County Pomona 10 in (25 cm)
Estell Manor 9 in (23 cm)
Atlantic City International Airport 8.3 in (21 cm)
Cape May County North Wildwood 10 in (25 cm)
Cape May City 8.5 in (22 cm)
Cape May Courthouse 8 in (20 cm)
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North Carolina

More information Location, Amount ...
Location Amount
Gastonia and New Bern 2 in (51 mm)
Jacksonville 4 in (100 mm)
Salisbury and Wilmington 5 in (130 mm)
Winston-Salem 7 in (180 mm)
Rocky Mount and Tarboro 8 in (200 mm)
Kannapolis 9 in (230 mm)
Charlotte, Greensboro, and Smithfield 10 in (250 mm)
Carrboro 14 in (360 mm)
Asheboro 15 in (380 mm)
Sanford, Chapel Hill, and Fayetteville 16 in (410 mm)
Durham 18 in (460 mm)
Monroe 20 in (510 mm)
Raleigh 24 in (610 mm)
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The Outer Banks received rain with the system and the mountains did not receive any precipitation.

Sources

  • "Second Guessing Mother Nature: Forecasting the Surprise Snow of January 2000". NASA Earth Observatory. NASA. Retrieved August 2, 2026.
  • "January 2000" (PDF). Storm Data and Unusual Weather Patterns. National Weather Service. Retrieved August 2, 2026.

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