found in the tropics between 30degreesN and 30degreesS
develop over oceans and lose energy over land
develop where the trade
winds are sucked towards the
equator because of the hot air
rising there.
sea temp must be above 26degrees celcius for atleast 60m below
surface. Humidity 75-80% this gives the right amount of heat and
water vapour to sustain the storm once started
wind speed must be above 120km/ph
Forms: rising warm air creates a low pressure zone,
sucks in more air, lots of moisture due to evaporation,
air rises and cools condensing into clouds, latent heat
energy released due to the transformation of vapour
into droplets heating the air even more.
Then, air rises even higher upto 10,000 m - this is the eye of
the storm. The spiralling rising air causes a huge column of
cumulonimbus clouds. When the air inside the hurricane
reaches the highest level it flows out of the eye a forms a broad
canopy of cirrus clouds.
The air cools and falls back down to sea level and is sucked back into
the centre. The Coriolis force cause the sucked in air at the bottom to
spin into the storm clockwise and the escaping air spins out
anticlockwise (opposite in the southern hem)
the formation of them is much rarer then the opportunities. 10% of falling pressure
centres give rise to them. In a year of high incidence perhaps a max of 50 will develop
but not all may cause disaster.
However, 2005 was a significant year for hurricanes in the north
atlantic with 20 forming and five reaching category 4 or 5. Including
hurricane Katrina , New Orleans USA.
size can vary from 100-1500km can form over a few days of 6-12 hours can last two-three days and take four to five to die out.
Destructive due to high winds and intense rainfall.
Tornadoes
A violent rotating column of air. Cone shaped cloud formation.
similar to tornadoes - whirl-winds, dust-devils(weaker
appearing over dry lands) and water spouts (tornado
over water)
numerous and devastating E.g. USA central, E and NE where an average five a day are reported in May.
Also common in Aus 15 a year but most fatalities in USA where
between 1950-78 689 t's where classed as deadly.
Can be viewed as miniature hurricanes, more common overland.
Form = warm moist air near the ground and dry air
above. E.g. Late spring early summer over the Great
Plains, USA. Intense heating of the ground make
warm moist air rise as it does it cools and makes
large cumulonimbus clouds.
The strength of the updraft (rising air) determines how much air is sucked into the bottom.
2 things help rotation:1) Coriolis force 2)high-level jet stream
passing across the top of the storm which gives an extra twist.
Because of the conditions required they can easily occur
under thunderstorms and hurricanes.
strength defined using 2 diff methods
Fujita (speed) and Pearson (length and
width of path) scale. Using these two you
can predict are affected and potential
damage.
Ice, wind, hail and snow storms
associated with either a polar front or high mountainous regions. They are worse in
winter. In northern hem common over N. America, Europe, Asia and Japan.
associated with depressions and violent mixing of warm and cold air masses.
SNOW = temp between the base of the cloud and ground must be below 4 degrees Celsius.
HAIL = Top of the storm must be very cold. In the reduced
pressure high up in the atmosphere, droplets supercooled to
less than zero degrees Celcius. They collide to form ice.
2mm to 20cm. The size is dependent on the updraft strength
as this determines how long they stay up in the atmosphere.
BLIZZARDS = worst storm conditions. They combine strong winds, driving snow, ice and hail with temps as low as 12 degrees Celsius and visibility less than 150 m.