December 2008 North American snowstorms

United States

Illinois

Chicago

Thick fog caused by the storms were responsible for flight cancellations in both the Chicago Midway Airport and the US's second busiest airport, O'Hare International Airport. On December 26, hundreds of flights were canceled. Operations began to return to normal the following day, though over a hundred flights were still canceled.

Oregon

Portland

The snowstorms were responsible for the greatest December snowfall in Portland, Oregon, in 40 years (the snowiest December in Portland was 1884, with more than 31 inches (79 cm) of snow). The City of Portland reported spending an estimated $2.17 million on snow removal, deicing of roads, and employee overtime due to the record snowfall.

Tri-Met suspended two-thirds of its bus lines. Hundreds of flights arriving and departing from Portland International Airport were canceled, leaving passengers and luggage stranded. Garbage services, privately run in the Portland area, were also canceled for over two weeks.

Washington

Seattle

The winter weather greatly affected the Seattle area, where snow brought the city to a standstill and temperatures reached record lows. Many holiday travelers were unable to reach their destinations when Greyhound canceled bus service, airlines canceled flights at Seattle–Tacoma International Airport, and Amtrak shut down passenger service between Eugene, Oregon, and Vancouver, British Columbia.

The city of Seattle was criticized over its response to the snowfall. Mayor Greg Nickels initially gave the city a "B" for its response to the snowstorm, but the director of the Department of Transportation admitted the city should have done things differently. The Seattle Department of Transportation did not use salt on the icy roads, opting instead to put sand and a chemical de-icer on the roads. The snowplows used by the city did not clear the roads entirely of snow, instead creating a hard snow-packed surface; this was done to minimize damage to the roads. The mayor later stated the city would use salt during future snowstorms, but the heavy criticism may have contributed to incumbent Mayor Nickels coming in third place in the next primary election.

Nevada

Las Vegas

A deep, upper-level trough had become established over the western United States during the weekend of December 13–14, 2008. Reanalysis data obtained online from Penn State University shows 700 mb temperatures across the area dropped to between −10 °C (14 °F) and −12 °C (10 °F) across southern Nevada by 06Z on December 14 and remained there through 12Z on December 17. An upper-level low moved southward along the West Coast of the United States, reaching the coast of southern California by 06Z on December 17. The low moved southeastward through the base of the upper-level trough axis and by the morning of December 17 was located along the coast of southern California. By 12Z on December 17, the low was accompanied by a 120+ knot jet stream that was located across the Mojave Desert (Figure 1). As the low approached southern California, the Mojave Desert was located under the left front quadrant of the jet, an area of typically favorable for lift. An area of diffluence, associated with this jet, was noted over southern California and western Arizona ahead of the upper low around 00Z on December 18, which also helped to further enhance lift across the area.

As a southwesterly flow aloft pushed moist air over the Mojave Desert, surface analysis indicated a north to northeast pressure gradient was also present in this area due to high pressure centered over eastern Utah. The 12Z sounding from Desert Rock (KDRA) indicated low-level northeasterly flow was present up through 850 mb with primarily southwesterly flow above that level (Figure 2). Between 12Z on December 17 and 00Z on December 18, a plume of subtropical moisture accompanied by precipitable water values of 0.30 to 0.50 of an inch was streaming northeastward toward the Mojave Desert. By 18Z on December 17, the jet stream had strengthened to 140 knots over Arizona, which placed southern Nevada near the left rear quadrant of the jet. Typically, the left rear quadrant of the jet corresponds to an area of subsidence, but in this case the curvature effects of the jet resulted in additional vertical motion in this quadrant. The upper low by then had moved towards the coast of southern California, with a distinct area of maximum Positive Vorticity Advection (PVA) at 500 mb having moved inland across the Mojave Desert (Figure 3).

Snow and a mix of snow and rain began to fall in the Las Vegas Valley shortly before 20Z on December 17. Radiosonde data from Desert Rock depicted warm advection took place between 12Z on December 17 and 00Z on December 18 with temperatures at 700 mb rising from −12 °C (10 °F) to −8 °C (18 °F) during that period. By around 02Z on December 18, precipitation generally became more intermittent as the area of maximum PVA had moved away from the area. Rain or a mixture of rain and snow tapered off between 05Z and 08Z on December 18 as warmer air finally infiltrated the lower levels and the upper low moved northeast over the Mojave Desert. Snow levels and amounts varied tremendously across the Las Vegas Valley with the greatest amounts located in the southeastern portion of the valley (Figures 4 and 5). Officially 3.6 inches of snow fell at the National Weather Service Office, which is located 2 miles southwest of McCarran International Airport. Generally 3 to 6 inches fell across the southern half of the valley. A maximum of 10 inches of snow was measured at the residence of a National Weather Service employee in southeast Henderson, near Railroad Pass, at an elevation of just under 2400 feet. The Henderson Executive Airport, located at an elevation of 2464 feet, in the southwestern part of Henderson received 8 inches. Snow amounts were highly variable along the famous Las Vegas Strip with the heaviest amounts on the southern end. At the “Welcome to Fabulous Las Vegas” sign on the far south end 1.7 inches of snow was measured while central and northern parts of The Strip saw snow barely coat some grassy surfaces and a few rooftops and metal objects at best. This corresponded well to a sharp-cut off noted overall across the center of the valley, where snow amounts decreased markedly. Across the northern half of the valley, snow levels were about 500 feet higher thus resulting in little to no snow accumulating here.