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7/31/2019 -Unlicensed-Atmospheric Disturbance NXPowerLite NXPowerLite
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AtmosphericDisturbances
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Thunderstorm
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Thunderstorm
Thunderstorms need three things:
Moistureto form clouds and rain.
Unstable Airrelatively warm air that can riserapidly.
Liftfronts, sea breezes and mountains arecapable of lifting air to help form
thunderstorms.
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Thunderstorm
Generating Seasons
1. Spring2. Summer
Occur during the afternoon and Evening
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Tornadoes
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Tornadoes
Natures most violent storms
Develop in all over the world but most
frequently in United States.
Generating seasons
1. Spring
2. Summer In an average 800 tornadoes reported every
year world wide.
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What causes tornadoes?
Tornadoes in the winter and early spring areoften associated with strong, frontal systems.
That form in the Central States and move east.
Occasionally, large outbreaks of tornadoesoccur with the following type of weatherpattern.
Warm, moist air advancing over the advancingcold front
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Facts of Tornadoes
The central vortex of a tornado is typically about328.1 ft (100 m) in diameter.
Wind speeds in the vortex have been measuredat greater than 220 mph (138 km/h).
These high winds make incredible feats ofdestruction possible.
They also cause the air pressure in the tornadoto drop below normal atmospheric pressure byover 100 millibars (the normal day-to-daypressure variations we experience are about 15millibars).
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Facts of Tornadoes
The air around the vortex is pulled into this lowpressure zone where it expands and cools rapidly.
This causes water droplets to condense from the air,making the outlines of the vortex visible as the
characteristic funnel shaped cloud. The low pressure inside the vortex picks up debris such
as soil particles, which may give the tornado anominous dark color.
A tornado can act as a giant vacuum cleaner sweepingover anything unlucky enough to be in its path.
The damage path of a tornado may range from 900 ft(300 m) to over 0.5 mi (1 km) wide.
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Facts of Tornadoes
Tornadoes move with the thunderstorm that theyare attached to, traveling at average speeds ofabout 10-30 mph (15-45 kph)
although some tornadoes have been seen tostand still, while other tornadoes have beenclocked at 60 mph (90 kph).
Since a typical tornado has a lifetime of about fiveto 10 minutes, it may stay on the ground for 5-10
mi (8-16km). Occasionally, a severe tornado may cut a path of
destruction over 200 mi (320 km) long.
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Facts of Tornadoes
Witnesses to an approaching tornado often
describe a loud roaring noise made by the
storm similar to jet engines at takeoff.
There is no generally accepted explanation for
this phenomenon although it has been
suggested that supersonic winds inside the
vortex cause it.
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Hurricane
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Hurricane: engine of destruction
Hurricanes are giant, spiraling tropical storms that canpack wind speeds of over 160 miles (257 kilometers) anhour and unleash more than 2.4 trillion gallons (9trillion liters) of rain a day.
These same tropical storms are known as cyclones inthe northern Indian Ocean and Bay of Bengal, and astyphoons in the western Pacific Ocean.
The Atlantic Oceans hurricane season peaks from mid-August to late October and averages five to six
hurricanes per year.
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Hurricanes begin as tropical disturbances inwarm ocean waters with surface temperaturesof at least 80 degrees Fahrenheit (26.5
degrees Celsius). These low pressure systems are fed by energy
from the warm seas.
If a storm achieves wind speeds of 38 miles(61 kilometers) an hour, it becomes known asa tropical depression.
Hurricane: engine of destruction
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A tropical depression becomes a tropical
storm, and is given a name, when its sustained
wind speeds top 39 miles (63 kilometers) an
hour.
When a storms sustained wind speeds reach
74 miles (119 kilometers) an hour it becomes
a hurricane and earns a category rating of 1 to5 on the Saffir-Simpson scale.
Hurricane: engine of destruction
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Hurricanes are enormous heat engines thatgenerate energy on a staggering scale. They drawheat from warm, moist ocean air and release itthrough condensation of water vapor in
thunderstorms. Hurricanes spin around a low-pressure center
known as the eye. Sinking air makes this 20- to30-mile-wide (32- to 48-kilometer-wide) area
notoriously calm. But the eye is surrounded by acircular eye wall that hosts the stormsstrongest winds and rain.
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These storms bring destruction ashore in
many different ways. When a hurricane makes
landfall it often produces a devastating storm
surge that can reach 20 feet (6 meters) highand extend nearly 100 miles (161 kilometers).
Ninety percent of all hurricane deaths result
from storm surges.
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A hurricanes high winds are also destructive and
may spawn tornadoes. Torrential rains causefurther damage by spawning floods and
landslides, which may occur many miles inland. The best defense against a hurricane is an
accurate forecast that gives people time to getout of its way. The National Hurricane Center
issues hurricane watches for storms that mayendanger communities, and hurricane warningsfor storms that will make landfall within 24 hours.
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