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Hurricane Winds

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Title: Hurricane Winds


1
Hurricane Winds
  • Mark Powell NOAA-AOML Hurricane Research
    Division

M. POWELL HURRICANE IMPACTS 2012
2
Measuring
A VARIETY OF SENSORS EXAMINE THE STORMS WIND
FIELD
M. POWELL HURRICANE IMPACTS 2012
3
Wind 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
4
Landfall
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
5
Landfall
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
6
Landfall 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
7
Post Landfall
KATRINA 10AM CDT
  • Pressure continues rising
  • Pressure gradient continues weakening
  • Enhanced friction diminishes the wind field

M. POWELL HURRICANE IMPACTS 2012
8
Storm 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
9
Wind 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
10
Hurricane 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
11
Hurricane Andrew 1992
M. POWELL HURRICANE IMPACTS 2012
12
Wind 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
13
Eyewall 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
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