Title: Hurricane Winds
1Hurricane Winds
- Mark Powell NOAA-AOML Hurricane Research
Division
M. POWELL HURRICANE IMPACTS 2012
2Measuring
A VARIETY OF SENSORS EXAMINE THE STORMS WIND
FIELD
M. POWELL HURRICANE IMPACTS 2012
3Wind Field
- Peak wind determines intensity
- Extent of damaging winds radii
- Projection of tropical storm winds relates to
evacuation
KATRINA 24 HOURS BEFORE LANDFALL
M. POWELL HURRICANE IMPACTS 2012
4Landfall
KATRINA 4 AM CDT
- Moving northward closer to land, storms
- Encounter cooler water on the continental shelf
- Interact with shear from approaching cold fronts
- Receive inflow of cooler, drier air flowing
offshore
M. POWELL HURRICANE IMPACTS 2012
5Landfall
KATRINA 7 AM CDT
- Pressure begins to rise
- Pressure gradient weakens
- Peak winds begin to decrease
- wind field expands conservation of angular
momentum
M. POWELL HURRICANE IMPACTS 2012
6Landfall Winds
KATRINA 7 AM CDT
- Structures and vegetation (roughness) slow down
the wind - Frictional Inflow increases
- Convergence zones can increase
- Gustiness (turbulence) increases
- Large wind differences between marine, open,
suburban areas
M. POWELL HURRICANE IMPACTS 2012
7Post Landfall
KATRINA 10AM CDT
- Pressure continues rising
- Pressure gradient continues weakening
- Enhanced friction diminishes the wind field
M. POWELL HURRICANE IMPACTS 2012
8Storm Decay
ANDREW 6 HOURS AFTER LANDFALL
- Cooler, drier air over land less fuel for the
heat engine - Stronger storms decay faster
- By 6 h after landfall, Andrew reduced from 140
kts to 95 kts
M. POWELL HURRICANE IMPACTS 2012
9Wind Damage
- Turbulence lofts missiles
- Complex terrain
- Local hilltops can double the wind
- Valleys and gorges can funnel the wind
- Wind tunnel modeling and flow models can help
identify risk areas
MISSILES LOFTED DURING HURRICANE INIKI ON LIHUE
(BRUCE ASATO, HONOLULU ADVERTISER)
HURRICANE MARILYN 1995 HILLTOP DAMAGE ON ST.
THOMAS
M. POWELL HURRICANE IMPACTS 2012
10Hurricane Tornadoes
- Mostly in outer bands
- Mostly front right
- Weaker than great plains types
- Difficult to detect
- Short life times, move quickly
- Additional damage microbursts
M. POWELL HURRICANE IMPACTS 2012
11Hurricane Andrew 1992
M. POWELL HURRICANE IMPACTS 2012
12Wind Damage
- Force goes with wind2
- Turbulence Cycling between gusts and lulls
causes fatigue - Roof suction pressures related more to turbulent
wind structure than peak wind - Wind direction houses experiencing winds from
many directions compared to one general direction
(eye vs eyewall) - Upstream terrain
M. POWELL HURRICANE IMPACTS 2012
13Eyewall Damage Hurricane Andrew
- Importance of construction details
- Strong building code
- Code enforcement and product approval
PHOTO POWELL, NARANJA LAKES AFTER HURRICANE
ANDREW
M. POWELL HURRICANE IMPACTS 2012