Tropical Cyclones Chapter 11 Meteorology 1010 Professor Bunds Utah Valley University
Tropical Cyclone Naming, Paths and Seasons typhoons hurricanes cyclones
Paths of All Tropical Cyclones
Hurricane Air Flow
Upper Level Hurricane Air Flow
Hurricane Rankings Saffir- Simpson Category Maximum sustained wind speed Minimu m surface pressure Storm surge mphm/sktsmbftm greater than less than
Hurricane Formation Powered largely by warm water Hurricanes are most common late summer to fall – ‘hurricane season’ –Varies by region Weaken over land –Usually weaken as they approach coastline also Form near but not over equator, given proper conditions (next slide)
Ingredients for Hurricane Formation Warm water – at least 80oF Relatively cool air at altitude Relatively moist air at moderate altitude (3 miles up) At least 300 miles from the equator Little wind shear between surface and upper air (6 miles up) Divergence aloft A trigger – e.g., big thunderstorms
Hurricane Hazards Storm Surge –On average, the biggest threat to life and property Winds Flooding from extreme precipitation –Can cause major problems far inland
Galveston Hurricane, 1900 > 10,000 fatalities, worst natural disaster in U.S. history
Storm Surge
Tropical Cyclone Winds & Storm Surge
Hurricane Ike Storm Surge September 2008
Hurricane Ivan 10 am Friday Link to visible loop
Hurricane Ivan 10 am Friday Link to visible loop
Hurricane Ivan 1:45pm Thursday
link to infrared loop
Hurricane Ivan 9:45pm Friday link to infrared loop
Hurricane Ivan 9:45pm Friday link to infrared loop
Link to visible loopLink to IR loop
Ivan, :15 am EDT
Ivan, :45 am EDT
Mississippi Delta
Mississippi River Delta Active Lobe ~ 500 years old Mississippi ‘wants’ to follow course of Atchafalaya River
Ivan, :15 pm EDT
Hurricane Ike Storm Surge September 2008
Path of hurrican and locations of tidal gauges that recorded storm surge, as shown on following slides
This and following photos are of Galveston, TX, and nearby areas
Houston, TX
High Island, Texas
Gilchrist, Texas
Orange, Texas