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Bill Sammler Warning Coordination Meteorologist National Weather Service Wakefield, VA VA Beach Summer Symposium - Hurricane Dynamics Winds, Storm Surge and Rainfall
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VA Beach Summer Symposium - Hurricane Dynamics

Jan 24, 2022

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Page 1: VA Beach Summer Symposium - Hurricane Dynamics

Bill SammlerWarning Coordination Meteorologist

National Weather Service – Wakefield, VA

VA Beach Summer Symposium - Hurricane

DynamicsWinds, Storm Surge and

Rainfall

Page 2: VA Beach Summer Symposium - Hurricane Dynamics

Let’s Start with Rainfall

Page 3: VA Beach Summer Symposium - Hurricane Dynamics

Track

Tropical Cyclone RainfallHurricane Irene – 2011 vs. Floyd - 1999

Page 4: VA Beach Summer Symposium - Hurricane Dynamics

Track

Tropical Cyclone RainfallHurricane Irene – 2011 vs. Isabel - 2003

Page 5: VA Beach Summer Symposium - Hurricane Dynamics

The Anatomy of the post-Matthew

Flood

Page 6: VA Beach Summer Symposium - Hurricane Dynamics

Overview• Third Significant Rainfall

Event in 6 weeks• Interaction with Cold Front

Enhanced Winds near the coast (SE VA/NE NC)– Matthew Not Truly Tropical

• Storm Surge/Beach Erosion a Problem

• Track Forecasts Were As Not Helpful in Assessing Potential Impacts As They Normally Are

Page 7: VA Beach Summer Symposium - Hurricane Dynamics

Hurricane Matthew Track

Page 8: VA Beach Summer Symposium - Hurricane Dynamics

Hurricane Matthew Rainfall

Track

Page 9: VA Beach Summer Symposium - Hurricane Dynamics

Salient Points• Widespread Major Floods

Rarely Result from a Single Heavy Rain Event

• Antecedent Moisture Conditions Play a Critical Role

• Heavy Rainfall in September Made Matthew’s Flooding Possible

• Rainfall Pattern Resulted in Unusual Impacts

Page 10: VA Beach Summer Symposium - Hurricane Dynamics

September Rainfall

Page 11: VA Beach Summer Symposium - Hurricane Dynamics

Hurricane Matthew Rainfall

Page 12: VA Beach Summer Symposium - Hurricane Dynamics

Where Does the Water Go?

Max Rainfall September through Matthew

Page 13: VA Beach Summer Symposium - Hurricane Dynamics

River Graph – Lawrenceville VA

Lawrenceville, VA -9/15 to 10/18

~2 ft.

~+20 ft.

~3 ft.~4 ft.

Page 14: VA Beach Summer Symposium - Hurricane Dynamics

River Graph – Franklin VA

Franklin, VA - 9/15 to 10/18

~+6 ft.

~+13 ft.

~1.0 ft.

~3.5 ft.

Page 15: VA Beach Summer Symposium - Hurricane Dynamics

Tidal vs. River Graphs

Page 16: VA Beach Summer Symposium - Hurricane Dynamics

Tidal vs. River Graphs

Page 17: VA Beach Summer Symposium - Hurricane Dynamics

Tidal vs. River GraphsSouth Mills, NC - 9/15 to 10/18

“Record” Stage

6 Days above

“record” stage!!

~6.5 ft.

~7.5 ft.

Page 18: VA Beach Summer Symposium - Hurricane Dynamics

Storm Surge Dynamics

Page 19: VA Beach Summer Symposium - Hurricane Dynamics

Storm Surge DefinitionSTORM SURGE – The abnormal rise in water

level directly associated with the wind and pressure forces associated with a hurricane

Storm Surge Example – hurricane makes landfall at high tide

Storm Surge is highest in right forward quadrant near center as it crosses coast

Wave effects, which cause most coastal damage, are not accounted for in storm surge measurements

Page 20: VA Beach Summer Symposium - Hurricane Dynamics

Storm SurgeStorm Surge Factors

• Storm Intensity and Size– Stronger = Higher Surge– Larger = Larger Area

Affected• Storm Speed

– Slower Often Means Higher Surge

• Angle to Coast at Landfall– Perpendicular Maximizes

Surge (Katrina)

Page 21: VA Beach Summer Symposium - Hurricane Dynamics

Katrina and Sandy Examples

Union Beach, NJ (blog, Spleeness)Long Beach, NJ (White House photo – Sonya Hebert)

Biloxi, MS (NOAA) Biloxi, MS (NOAA)

Page 22: VA Beach Summer Symposium - Hurricane Dynamics

Storm Surge

Storm Surge is highest and

Winds are greatest in the RIGHT FORWARD

QUADRANT close to where center makes landfall

Storm Surge vs. Location Relative to Storm

Page 23: VA Beach Summer Symposium - Hurricane Dynamics

Storm Surge ExampleFACTOR = STORM DIRECTION

CAT 2 Max Surge

CAT 2 NE 20 mph

Page 24: VA Beach Summer Symposium - Hurricane Dynamics

Storm Surge ExampleFACTOR = STORM DIRECTION

CAT 2 Max Surge

CAT 2 N 20 mph

Page 25: VA Beach Summer Symposium - Hurricane Dynamics

Storm Surge ExampleFACTOR = STORM DIRECTION

CAT 2 Max Surge

CAT 2 WNW 20 mph

Page 26: VA Beach Summer Symposium - Hurricane Dynamics

Hurricane Winds

Page 27: VA Beach Summer Symposium - Hurricane Dynamics

Hurricane Wind Characteristics

• Strongest along the coast/over water, and near the center of well developed systems– Weaker/weakening systems have more chaotic

wind field

• Systems becoming non-tropical are the most difficult to forecast relative to winds (e.g Matthew – 2016)

• Hampton Roads has not experienced true hurricane winds in decades

Page 28: VA Beach Summer Symposium - Hurricane Dynamics

Hurricane Irene (2011) Winds

Page 29: VA Beach Summer Symposium - Hurricane Dynamics

Matthew Peak Gusts

Matthew plus Cold Front

Matthew only

Page 30: VA Beach Summer Symposium - Hurricane Dynamics

The End!!Are There Any Additional

Questions?

[email protected]