HURRICANE (TYPHOON) DEVELOPMENT CONDITIONS FOR HURRICANE DEVELOPMENT: 1. OCEAN TEMPERATURE MUST...

20

Transcript of HURRICANE (TYPHOON) DEVELOPMENT CONDITIONS FOR HURRICANE DEVELOPMENT: 1. OCEAN TEMPERATURE MUST...

Page 1: HURRICANE (TYPHOON) DEVELOPMENT CONDITIONS FOR HURRICANE DEVELOPMENT: 1. OCEAN TEMPERATURE MUST EXCEED 27EC WARM WATER PROVIDES THE ENERGY SOURCE FOR.
Page 2: HURRICANE (TYPHOON) DEVELOPMENT CONDITIONS FOR HURRICANE DEVELOPMENT: 1. OCEAN TEMPERATURE MUST EXCEED 27EC WARM WATER PROVIDES THE ENERGY SOURCE FOR.

HURRICANE (TYPHOON) DEVELOPMENT

CONDITIONS FOR HURRICANE DEVELOPMENT:

1. OCEAN TEMPERATURE MUST EXCEED 27C

WARM WATER PROVIDES THE ENERGY SOURCE FOR THE SUSTENANCE OF THE HURRICANE

2. LATITUDE MUST BE > 4 N BUT < 15

(WATER IS TOO COLD > 15 )

3. WARM WATER MUST REACH DEPTHS OF ~ 100 M

I.E. ENERGY STORED NEEDED TO SUSTAIN STORM

Page 3: HURRICANE (TYPHOON) DEVELOPMENT CONDITIONS FOR HURRICANE DEVELOPMENT: 1. OCEAN TEMPERATURE MUST EXCEED 27EC WARM WATER PROVIDES THE ENERGY SOURCE FOR.

Atlantic hurricanes often develop off Cape Verdeor in Caribbean or Gulf of Mexico.

Typhoons are Pacific Hurricanes.

Page 4: HURRICANE (TYPHOON) DEVELOPMENT CONDITIONS FOR HURRICANE DEVELOPMENT: 1. OCEAN TEMPERATURE MUST EXCEED 27EC WARM WATER PROVIDES THE ENERGY SOURCE FOR.

HURRICANE CHARACTERISTICS AND ORIGINS:

A. MOST HURRICANES REACHING THE USA START AS"CAPE VERDE" STORMS

CAPE VERDE STORMS ARE AREAS OF CONVECTIVESTORMS THAT FORM OFF THE NORTHWEST COASTOF AFRICA AND PROPAGATE INTO THE ATLANTIC

B. HURRICANES NEVER OCCUR IN SOUTH ATLANTIC,AS THE WATER IS TOO COLD

C. HURRICANES MAY FORM IN THE CARIBBEAN

D. PACIFIC HURRICANES = TYPHOONS CAN REACHHIGHER STRENGTHS (WIND VELOCITIES) AND LIVELONGER THAN ATLANTIC HURRICANES

E. HURRICANE MOVEMENTS ARE UNPREDICTABLEAND ARE COUPLED TO MOVEMENTS OF OTHERWEATHER SYSTEMS, E.G. WAVE CYCLONES

Page 5: HURRICANE (TYPHOON) DEVELOPMENT CONDITIONS FOR HURRICANE DEVELOPMENT: 1. OCEAN TEMPERATURE MUST EXCEED 27EC WARM WATER PROVIDES THE ENERGY SOURCE FOR.

HURRICANES ARE A HEATENGINE, TRANSFERRING HEAT FROM THE OCEAN TO THEATMOSPHERE.

HEAT COMES IN VIA WARMWATER AND IS EXHAUSTEDOUT THE TOP INTO THEUPPER TROPOSPHERE ANDLOWER STRATOSPHERE.

SOME AIR SINKS INTO THE“EYE” OF THE STORMCREATING CLEAR AND CALMCONDITIONS.

Page 6: HURRICANE (TYPHOON) DEVELOPMENT CONDITIONS FOR HURRICANE DEVELOPMENT: 1. OCEAN TEMPERATURE MUST EXCEED 27EC WARM WATER PROVIDES THE ENERGY SOURCE FOR.

DIVERGENCE

Page 7: HURRICANE (TYPHOON) DEVELOPMENT CONDITIONS FOR HURRICANE DEVELOPMENT: 1. OCEAN TEMPERATURE MUST EXCEED 27EC WARM WATER PROVIDES THE ENERGY SOURCE FOR.
Page 8: HURRICANE (TYPHOON) DEVELOPMENT CONDITIONS FOR HURRICANE DEVELOPMENT: 1. OCEAN TEMPERATURE MUST EXCEED 27EC WARM WATER PROVIDES THE ENERGY SOURCE FOR.

WIND SPEED PROFILE ACROSS A TYPICAL HURRICANE

EYE

Page 9: HURRICANE (TYPHOON) DEVELOPMENT CONDITIONS FOR HURRICANE DEVELOPMENT: 1. OCEAN TEMPERATURE MUST EXCEED 27EC WARM WATER PROVIDES THE ENERGY SOURCE FOR.

Highest winds and greatest tidal surge occur to the side with both forward and circular wind velocity adding together.

Page 10: HURRICANE (TYPHOON) DEVELOPMENT CONDITIONS FOR HURRICANE DEVELOPMENT: 1. OCEAN TEMPERATURE MUST EXCEED 27EC WARM WATER PROVIDES THE ENERGY SOURCE FOR.

CHANGED OCEAN LEVELS DURING APPROACH OF A HURRICANE (NORTHSIDE)

Page 11: HURRICANE (TYPHOON) DEVELOPMENT CONDITIONS FOR HURRICANE DEVELOPMENT: 1. OCEAN TEMPERATURE MUST EXCEED 27EC WARM WATER PROVIDES THE ENERGY SOURCE FOR.

Hurricane Katrinamay now be third onthis list in loss of life.

Page 12: HURRICANE (TYPHOON) DEVELOPMENT CONDITIONS FOR HURRICANE DEVELOPMENT: 1. OCEAN TEMPERATURE MUST EXCEED 27EC WARM WATER PROVIDES THE ENERGY SOURCE FOR.

RADAR ECHOES SHOWING RAINFALL IN H. ANDREW

Page 13: HURRICANE (TYPHOON) DEVELOPMENT CONDITIONS FOR HURRICANE DEVELOPMENT: 1. OCEAN TEMPERATURE MUST EXCEED 27EC WARM WATER PROVIDES THE ENERGY SOURCE FOR.

RICHELIEU APARTMENTS BEFORE H. CAMILLE

Page 14: HURRICANE (TYPHOON) DEVELOPMENT CONDITIONS FOR HURRICANE DEVELOPMENT: 1. OCEAN TEMPERATURE MUST EXCEED 27EC WARM WATER PROVIDES THE ENERGY SOURCE FOR.

RICHELIEU APARTMENTS AFTER H. CAMILLE

Page 15: HURRICANE (TYPHOON) DEVELOPMENT CONDITIONS FOR HURRICANE DEVELOPMENT: 1. OCEAN TEMPERATURE MUST EXCEED 27EC WARM WATER PROVIDES THE ENERGY SOURCE FOR.

Hurricane Isabel

CLOUD HEIGHTS AROUND H. ISABEL: ORANGE HIGHEST (COLDEST)

Page 16: HURRICANE (TYPHOON) DEVELOPMENT CONDITIONS FOR HURRICANE DEVELOPMENT: 1. OCEAN TEMPERATURE MUST EXCEED 27EC WARM WATER PROVIDES THE ENERGY SOURCE FOR.

PROJECTED PATH ISUNCERTAIN

Page 17: HURRICANE (TYPHOON) DEVELOPMENT CONDITIONS FOR HURRICANE DEVELOPMENT: 1. OCEAN TEMPERATURE MUST EXCEED 27EC WARM WATER PROVIDES THE ENERGY SOURCE FOR.

CONTINENTAL WEATHER PATTERNSINFLUENCE TRACKS OF HURRICANES

Page 18: HURRICANE (TYPHOON) DEVELOPMENT CONDITIONS FOR HURRICANE DEVELOPMENT: 1. OCEAN TEMPERATURE MUST EXCEED 27EC WARM WATER PROVIDES THE ENERGY SOURCE FOR.
Page 19: HURRICANE (TYPHOON) DEVELOPMENT CONDITIONS FOR HURRICANE DEVELOPMENT: 1. OCEAN TEMPERATURE MUST EXCEED 27EC WARM WATER PROVIDES THE ENERGY SOURCE FOR.
Page 20: HURRICANE (TYPHOON) DEVELOPMENT CONDITIONS FOR HURRICANE DEVELOPMENT: 1. OCEAN TEMPERATURE MUST EXCEED 27EC WARM WATER PROVIDES THE ENERGY SOURCE FOR.

TS Alpha, and on 31 October, 2005, Hurricane Beta and eventually, HurricaneGamma formed.

This was the all time record TS and Hurricaneseason for the Atlantic since 1851.