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Winter Storms and Northeasters. Robert E. Davis. Dept. of Environmental Sciences. University of Virginia. Email: red3u@virginia.edu. Virginia Mitigation Summit June 17, 2004. Nor’easters and Snowfall in Virginia. Nor’easters. Snow. Nor’easter- generated snowfall.
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Winter Storms and Northeasters Robert E. Davis Dept. of Environmental Sciences University of Virginia Email: red3u@virginia.edu Virginia Mitigation Summit June 17, 2004
Nor’easters and Snowfall in Virginia Nor’easters Snow Nor’easter- generated snowfall Many Virginia snow events are not linked to nor’easters
H Cold Air Cold Air Damming WINTER STORM INGREDIENTS Cold Air Damning 1. Sufficient cold air source
WINTER STORM INGREDIENTS Moist Air 2. Sufficient moisture Moist Air
WINTER STORM INGREDIENTS winds L 3. Lifting mechanism (the “storm”)
Cold Air WINTER STORM INGREDIENTS H L Moist Air
Cold Air L TIMING IS EVERYTHING H *Arrival of storm does not coincide with cold air *Warm air from Atlantic decreases vertical thickness of cold air mass
TIMING IS EVERYTHING L L *Forward speed too fast *Low snow accumulations
WINTER STORM INGREDIENTS L L L *Track too far inland *Not enough moisture
THE “SNOWMAKER” TRACK *Ideal track for producing snow in the Mid-Atlantic Heaviest snow frequency * * * Storm Track (Knappenberger and Michaels, 1993)
NOR’EASTERS “A cyclonic storm of the east coast of North America, so called because the winds over the coastal area are from the northeast” (Glossary of Meteorology) L *New England *gale force winds *winter *high waves *beach erosion
FACTORS THAT DETERMINE WAVE HEIGHTS IN DEEP WATER *wind speed *wind duration *fetch Wave height climatologies can be “hindcasted” from historical weather records
Wave Approach Fetch Storm Center
Nor’easter Type by Class I IV Most Class IV and V storms form near the Bahamas or Florida II V III
1. New England High • Cold air source • Slows forward motion of storm H • 2. Coastal storm • Atlantic moisture • Lifting mechanism • Slow movement = more snow • Slow movement = bigger waves L L L L NOR’EASTERS AND VIRGINIA SNOW Most major snowstorms in Virginia are caused by large nor’easters
JET STREAM 1) Boundary between warm, tropical and cold, polar air masses 2) Size and strength vary seasonally 3) Linked to mid-latitude storms at surface 4) Linked to storm tracks
IN WINTER, JET STREAM 1) EXPANDS 2) STRENGTHENS JANUARY JULY
PREFERRED WINTER STORM TRACKS L L L L L L Continental Track L L Coastal Track L L (After Hayden, 1981)
Golfer’s track “Snowmaker” track (Knappenberger and Michaels, 1993)
H ASH WEDNESDAY STORM March, 1962 • Strong high to north • Storm track off coast • (Bahamas Low) • Slow-moving • Strong northeast winds to the • north of storm • Long fetch, strong winds from same • direction for long duration
ASH WEDNESDAY STORM, MARCH, 1962 Snowfall (inches)
“STORM OF THE CENTURY” March, 13 1993; 7 a.m. EST
“Storm of the Century” Surface weather map 3/13/1993 7 p.m., EST
EL NINO AND VIRGINIA PRECIPITATION LA NINA EL NINO
EL NINO AND VIRGINIA TEMPERATURE LA NINA EL NINO
EL NINO AND VIRGINIA SNOWFALL 35 El Nino La Nina 30 25 20 VIRGINIA SNOWFALL (INCHES) 15 10 5 0 -8 -6 -4 -2 0 2 4 JAN-MAR EL NINO STATUS
Winter Storms and Northeasters Robert E. Davis Dept. of Environmental Sciences University of Virginia Email: red3u@virginia.edu Virginia Mitigation Summit June 17, 2004 Thanks to: Chip Knappenberger Jerry Stenger Pat Michaels