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science gr8 3rd qtr
typhoon
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Weather
Condition of the atmosphere at a specific place and time
Located in the
troposphere
, the
lowest
layer of the atmosphere
Weather Disturbance
Disruption in the
steady state
of the atmosphere
Common disturbances include
storms
,
thunderstorms
,
tornadoes
, and
tropical cyclones
Caused by interactions between
hot
and
cold air masses
Typhoon Development
Water
evaporates at ocean surface (
26.5°C
).
Warm
,
moist
air rises, creating
low
pressure.
Cool
air rushes in,
heating up
and carrying more
vapor.
Rising
warm
air cools,
condensing
into
clouds.
Wind spirals due to
Coriolis effect
, forming a
typhoon.
When this happens storms, thunderstorms, tornadoes, hurricanes, or tropical cyclones occur.
TYPES OF WEATHER DISTURBANCES
STORM
THUNDERSTOM
HURRICANE
STORM
Violent disturbance
in atmosphere.
Marked by
sudden air pressure
changes.
Features
rapid air movements.
Varies in
size
and
scope.
THUNDERSTORM
Localized storm cloud.
Generates
thunder
and
lightning.
Brings heavy rain
,
strong winds
,
lightning
, and
thunder.
Intense
,
localized weather event.
HURRICANE
Tropical storm.
Diameter
around
100
m.
Spiraling winds 120
to
300
kph.
Intense tropical cyclone.
Formed over
warm ocean waters.
Can cause
extensive damage.
HURRICANE vs CYCLONE
Formed in
Atlantic
or
Central Pacific
:
HURRICANE
Formed over
Indian
Ocean:
CYCLONE
Hurricane Eye
Center
of the storm
Moves
counterclockwise
Calmest
part
Surrounded by
eyewall
Tropical
Cyclones
Forms over
warm water
Large
,
powerful storm
Tropical Depression
(TD)
Heavy rainfall
Max wind up to 61 kph
Tropical Storm
(TS)
Strong thunderstorms
Wind:
62-88 kph
Severe Tropical Storm (STS)
Wind:
89-117
kph
Typhoon
Max wind
:
118-220
kph
Eye
develops
Super
Typhoon
Wind exceeds
220 kph