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Nature of tropical storms and their causes
1. HayleyPower12I
Tropical StormsResearch
TheNatureof TropicalStorms andTheirCauses
What are they?
A very intense lowpressure weather system that can last for weeksin the tropical regions
of the planet
Spinsdue to the Coriolis of the earth’sspin (the earth is widest (40,000 km)atthe equator
andtravels 1,700km/h, however, at60° NorthandSouth ofthe equatorit's only half thesize
so travels halfasfast. This meanswind is deflected rightinthenorthernhemisphere andleft
in the southernhemisphere. This deflection causesthe tropical stormsto rotate).
They rotate clockwise towardsthe south west inthesouthernhemisphereand anticlockwise
towardsthe northwest inthenorthernhemisphere
Also knownas Hurricanes (northAmerica), Cyclones (India)andTyphoons (JapanandEast
Asia)
Facts
In a normalyear over a dozen hurricanesfromoverthe Atlantic ocean
They head westward towardtheCaribbean, theeast coast of Central America and Southern
USA (especially Florida)
They can last upto a month
Travel quite slowly (15mph)
Wind speedscan reach 75mph
Mostcommonbetween May andDecember inthenorthernhemisphere
Mostcommonbetween November andApril inthesouthern hemisphere
Where do they happen?
A bandthatlies between the tropics of Cancer andCapricorn
Sea temperature 27°C andabove
Sea over 60m deep
Mosteffected area is South East Asia, whichhasaround 26 stormsayear
Least effected area is India, withonly 2 stormsayear
Naming
They havebeen named since the early 1950s toavoidconfusionand streamline
communications
1953: femalenames
1978: maleandfemale names(Northern pacific)
1979: aboveadoptedby Atlantic
Alternate between male and female names
Go throughthe alphabetrestarting with A at the startof each year (excluding Q, U, X, Y and
Z)
2. HayleyPower12I
Tropical StormsResearch
Why do they happen?
1. Warm, wet air rises andcondensesto from clouds (and heavy rainfall) aswell as a low
pressure zoneon the surface of the water
2. The warm rising air causes the pressureto decrease at higher altitudes. The warm air I under
a higher pressure thanthe cold air somovestowards the space occupiedby the colder air.
The low pressure“sucksin” air from the surroundingswhich also rises, creating more clouds
andrain
3. Air surrounding thelow pressure zone flows in a spiral at highspeeds
4. Air is ejected at the top of the storm(can be 15kmhigh)andfalls to the outsideof the storm,
away from the eye. This reduces the massof the air over the eye, further increasing wind
speeds. Somealso cools, dries andsinks(adding to the low pressure).
5. The faster the wind blows, the lower the pressurein the centre (so the hurricane gets
stronger)
6. Fromabove, hurricanes can be seen as huge circular bodiesof thick clouds about 450km
wide. These clouds bring heavy rain, thunderand lightning
7. In the centre is the eye. Itis about45kmacross. Thereare no clouds, weak winds andlittle to
no wind as cold air is descending
8. As hurricanes moveinshore they lose energy as they can nolonger draw it from the sea and
eventually die
Structure
Eye Eye wall Edge of storm Surrounding area
Calm weather Warm moistair spirals
upwards
Lighter rain and winds Air suckedin
Stormsurge at highest
point
Heavy rain
Strongwinds
Effects
Primary
Electricity cables damaged
Livestock killed
Coastalhabitatsdamaged
Flooding
Buildings, bridges, homesetc. damaged
Injuries/lossof life
Secondary
Shortageof food
Rise in unemployment
Diseases spreaddue to shortagesof clean water
3. HayleyPower12I
Tropical StormsResearch
Emergency services can't get throughdue to blockedroads
People left homeless
Psychologicalproblems
Responses
Before
Build a sea wall (prevent flooding from stormsurge)
Evacuate people
Educate people
Build onsafe zones
During
Emergency services
Shelters
Aid
After
Rebuildingdamaged buildings
Makinghomes/buildingsstronger
Case study
Hurricane Katrina (morelikehurricanetortilla) –see flashcards
Sources
http://www.coolgeography.co.uk/A-
level/AQA/Year%2013/Weather%20and%20climate/Hurricanes/Tropical%20Storms.htm
https://www.bbc.com/bitesize/guides/z37wrdm/revision/1