NATS 101 Lecture 28 Lightning
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Transcript of NATS 101 Lecture 28 Lightning
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NATS 101
Lecture 28Lightning
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Review: Thunderstorms
• A cumulonimbus with lightning and thunder!• Deep layer of conditionally unstable air is
necessary to produce a thunderstorm. • Several types of thunderstorms.
Single Cell, Multicell, Squall Line, Mesoscale Convective Complexes, Supercells
• Pose major hazards to public and economy.
Lightning, Hail, Microburst Winds, Flash Flooding, Tornadoes
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Lightning Basics
• What is lightning?
An electric discharge, or spark, that occurs in thunderstorms (usually)
80% occurs within clouds
20% occurs between cloud and ground
• Lightning is ubiquitous, with more than 6,000 ground strikes per minute from 40,000 thunderstorms per day worldwide
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Lightning Videos
• Examples were shown of
In-Cloud (IC) Lightning
Cloud-to-Cloud (CC) Lightning
Forked LightningIC Lightning Video from MetEd/UCAR
• MCC Lightning from Space ShuttleLightning from Space Video from NASA
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Lightning Pictures
• Examples were shown of
Cloud-to-Ground (CG) Lightning
In-Cloud (IC) Lightning
Cloud-to-Cloud (CC) Lightning
Forked LightningChuck Doswell's Lightning Pictures-Very Nice!
• Excellent photography tips can be found at Chuck Doswell’s web site. He’s good!
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Cloud-to-Ground Lightning
www.nssl.noaa.gov/~doswell/ltgph.html
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In-Cloud Lightning
www.nssl.noaa.gov/~doswell/ltgph.html
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Forked Lightning
www.nssl.noaa.gov/~doswell/ltgph.html
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Charge Separation
Lightning requires the separation of different charges into different regions of a cloud.
How does charge separation in clouds occur?We don’t know for certain, but we observe this:
Lightning only occurs in cold clouds with supercooled droplets and temps below 5oF.
Thus, the ice crystal processes responsible for precipitation in cold clouds likely plays an critical role in charge separation.
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Charge Separation: One Theory
Hailstones are covered by a layer of liquid water.
The thin layer of liquid is positively charged.
When hailstones and ice crystals collide, some of liquid molecules stick to the ice crystals.
Along with the mass transfer, positive ions transfer from the hailstones to the ice crystals.
The heavier, negative hail falls to cloud bottom.
The lighter, positive ice crystals drift to cloud top.
Produces negative lower, positive upper cloud.
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Charge Separation
• Top of cloud top has a positive charge.
• Lower and middle of cloud has a negative charge.
• Charge separation in cloud maintains the earth’s fair weather electric field denoted by the arrow E
• E points toward positive polarity
Williams, The Weather Book
PolarizationPolarization
––
++
E
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• An electric potential exists between the ionosphere (positive) and surface (negative)
• Potential varies between 200,000 - 500,000 Volts
• Average current is 2x10-12 Amps/m2
• Power is 10-6 W/m2
Fair Weather Electric Field
www://thunder.msfc.nasa.gov/primer
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Lightning StrokeCloud-Ground Sequence
1) Downward stepped leader. Stepped leader is invisible.
2) Upward return stroke.
3) Downward dart leaders.
4) Upward return strokes.
Dart leaders-return strokes: up to 25 cycles, 3-4 usually.
Ground strikes are usually negative, that is electrons flow from cloud to ground.
Williams, The Weather Book
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www://thunder.msfc.nasa.gov/
Types of Discharges
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Lightning Safety
Williams, The Weather Book
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Thunder
What Causes Thunder?• Lightning rapidly heats air
to more than 30,000oC.• The intense heating causes
the air to expand rapidly. • The expanding air cools,
then contracts rapidly. • The expansion-contraction
generates sound waves.
Williams, The Weather Book
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How Far Away Is It?
• We see lightning instantly.• But sound travels 1,000 ft
every second. If you hear thunder 10 seconds after seeing lightning, the bolt is 2 miles (~10,000 ft) away.
• We hear thunder from closest part of flash first, farthest part last. This causes the rumble sound.
Williams, The Weather Book
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Why Thunder Rumbles?
• Assume that you are one mile away from a a one mile long bolt.
• You hear thunder from the lower part of flash in 5 seconds, from the upper part of flash 7 seconds.1 mile
5 seconds
1 m
ile
1.4 miles
7 seconds
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National Lightning Detection Network
thunder.msfc.nasa.gov/primer
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www.nssl.noaa.gov/western/kaney
Tucson
Phoenix
FlagstaffGallup
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Tucson
Phoenix
www.nssl.noaa.gov/western/kaney
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Global Lightning Distribution from Satellite, Take 2
www.msfc.nasa.gov
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Let’s Play “Who Gets Toasted”
• What is the probability in Tucson of a Cloud-to-Ground lightning stroke hitting within a certain Radius R of you in an “average” year?
• Guesses? No peeking!
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Courtesy Prof. E.P. Krider
Dept. of Atmospheric Sciences
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CG Lightning over Tucson(2000-2002)
• 65,000 flashes in 80 km 80 km over 3 years
~3.3/km2 per year• Much higher
during monsoon ~12/km2 per year
Courtesy Prof. E.P. Krider Dept. of Atmospheric Sciences
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Summary: Key Points
• Lightning - electric discharge in thunderstorms 80% within clouds, 20% cloud to ground
• Lightning is ubiquitous, with more than 6,000 cloud-to-ground strikes per minute from more than 40,000 thunderstorms per day worldwide.
• Lightning requires the separation of different charges into different regions of cloud.
• Charge separation maintains the earth’s fair weather electric field.
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Assignment for Next Lecture
• Topic - Tornadoes • Reading - Ahrens, p277-290• Problems - 10.25, 10.26, 10.29