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8/7/2019 Winter Weather (Paul Kocin)
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Winter Storms
by
Paul Kocin
Winter Storm Expert
The Weather Channel
and
Dr. Gerry Bell
Climate Prediction Center
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Outline1. Winter Weather Impacts
2. Winter Forecast Issues
3. Northeastern U.S. Snowfall Impact Scale
4. Climate factors influencing winter storms
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Winter Weather Impacts
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Each year, automobile accidents claim an incredible amount
of lives, cause injuries and property damage.
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The average/year of auto accidents:
41,000 deaths,
3 million injuries, billions in damage.
About 15% is weather-related
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Weather related:
7,000 deaths
800,000 injuries
and billions of dollars in damage per year!
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Adverse weather is associated with over 1.5 million autocrashes per year.
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Snowandice make up a significant component ofthe
dangersposedtotransportationnationwide.
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Examples: In 2001
5400 deaths linked to rain-slicked roads 1100 deaths linked to snowand ice
670 deaths linked to fog
Dept. of transportation cost estimates Injuries, loss of life, and property damage
cost an average of 42 billion dollars
annually just for snowand ice!
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Winter Forecast Issues
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Winter forecast issuesPrecipitation type forecasts can be very difficult, especially
a day or more into the future
Rain vs freezing rain vs sleet vs snow
Model forecast uncertainty:
Different models can often show significantly different
forecasts beyond a few days.
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The main issue: rain vs freezing rain vs sleet
vs snow
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Predictability
Some storms are easy.
Affect one small region its well forecast
Life is GREAT
Most storms are widespread, multi-day, multi-formevents..forecasts can be good one place,
Lousy others
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More predictability
Whether big or small, winter storm predictability is very
variable.
Some winter storms are amenable to prediction even
several days in advance
Other winter storms seem to be unpredictable even up to
the day of the event
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Mean= 4.80
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5 TopRankedSnowfall Events
Rank DATE NESIS
1 12-14 MAR1993 12.52 2 6-8 JAN 1996 11.54
3 15-18 FEB 2003 8.91
4 11-14 MAR1888 8.34
5 11-14 FEB 1899 8.11
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Nor
theas
tSnowfa
ll
Impact Scale
(NESIS)
Paul J. Kocin & LouisUccellini
The
Wea
ther
Channe
l & NWS/
NCEP
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Measure potential for
DESTRUCTION to property
and loss of life from
tornadoes and hurricanes
Fujita and Saffir-Simpson Scales
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Measurespotential forhumanandeconomic
DISRUPTION
Categories(1thru5)
NESIS
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SNOWFALL
WINDSPEED
TEMPERATURE
DURATION
SNOWFALL RATES STORM INTENSITY
GROUND TEMPERATURES
SNOWSTORM IMPACTDUE TO:
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A measure that is based on the integratedeffects of storm snowfall in the NortheastUnited States
What NESISis
Based on areal coverage of snowfall
amounts and population affected
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LOOKED AT 30 CASES
1950-2000
CONTOUREDSNOWFALL
at 4, 10and at
20 intervals
THOSE CONTOURS
REPRESENT:
(1) anAREA(2) anAFFECTED POPULATION
Feb 1978
Mar1993
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Mostly 4-10, small 10+
NESIS VALUES
Close to1
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Small 4, Largerareaof10+, small 20+
NESISVALUES
Closeto3
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Evenlargerareaof4+, 10+, 20+
NESIS VALUES
Greaterthan8
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NESISCATEGORIES
CATEGORY NESISVALUES # of CASES DESCRIPTION
1 1 2.499 23 NOTABLE
2 2.5 - 3.99 22 SIGNIFICANT
3 4 5.99 16 MAJOR
4 6 - 9.99 7 CRIPPLING 5 10.0 + 2 EXT REME
Being tested at NCDC for possible
NWS operational use
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Climate Factors Influencing Winter Storms
1. El Nio/ La Nia cycle
2. North Atlantic Oscillation
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El Nio and La Nia
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SST(C) and Departures
28oC is approximate threshold for deep tropical convection
28 28
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ENSO Tropical Rainfall
El Nio: Tropical convection, jet stream extended eastward
La Nia: Tropical convection, jet stream retracted westward
EL Nio
Enhanced
Convection
La Nia
suppressedconvection
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El Nio:
Extended Jet Stream
More zonal flow over U.S.
South shift of storm track
Weaker Hudson Bay Low
Fewer arctic outbreaks
La Nia:
Retracted Jet Stream
More meridional flow
Blocking over N. Pac
Stronger Hudson Bay Low
More arctic outbreaks
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North Atlantic Oscillation (NAO)
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NAO Air Pressure and Winds
at 30,000 ft
1980s- 2001 1950s-1960s
++-
-
NAO affects the Atlantic jet stream/ storm trackNAO affects the Atlantic jet stream/ storm track
Tremendous differences in poleward heatTremendous differences in poleward heat
transporttransport and temperatures at high latitudesand temperatures at high latitudes
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Positive (warm) Phase of Wintertime NAO
Temperature Precipitation
Warmer Colder Wetter Drier
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NAO: DJF Time Series
50
55
60
6570 7
580 8
5
90
9500
Positive: 1980s-present
Weaker Hudson Bay Low
Arctic air confined to Canada
Milder Temperatures
Negative: 1950s-1960s
Stronger Hudson Bay Low
More Arctic outbreaks
Cooler Temperatures
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Moderate-to-Strong
El Nios
Negative NAO:
Cooler in SE,
Mid-Atlantic, NE
Positive NAO:
Warmer in SE,
Mid-Atlantic, NE
El Nio NAO
Temperature Composites
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Daily NAO Index
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