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2006 PQIG Workshop The Physics of Lightning Michael F. Stringfellow
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Page 1: 2006 PQIG Workshop The Physics of Lightning Michael F. Stringfellow.

2006 PQIG Workshop

The Physics of Lightning

Michael F. Stringfellow

Page 2: 2006 PQIG Workshop The Physics of Lightning Michael F. Stringfellow.

2006 PQIG Workshop

Introduction

The Physics of Lightning:• How lightning originates• Leader propagation• Strike mechanism• The return stroke• Subsequent strokes• Channel multiplicity• Lightning flash density• Lightning interaction with overhead power lines

Page 3: 2006 PQIG Workshop The Physics of Lightning Michael F. Stringfellow.

2006 PQIG Workshop

The Thundercloud

Page 4: 2006 PQIG Workshop The Physics of Lightning Michael F. Stringfellow.

2006 PQIG Workshop

How Lightning Starts

•Lightning starts in cloud– Around 0°C - that’s

typically 15,000 ft above ground

– Breakdown starts in high-field region

– Branching discharge moves up and down

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Page 5: 2006 PQIG Workshop The Physics of Lightning Michael F. Stringfellow.

2006 PQIG Workshop

Leader Propagation

•Ground flashes almost always start with downward (usually) stepped leader from high charge region•Steps 10-100 m long•Pauses between steps•Lowers charge to earth• Negative in > 95% of ground flashes

Breakdown zone

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- -- -

- -

--

Page 6: 2006 PQIG Workshop The Physics of Lightning Michael F. Stringfellow.

2006 PQIG Workshop

Connecting Leaders

•Launched upward by electric field of stepped leader as it approaches earth•Occur at many locations near descending flash•Most are unsuccessful•One or more connect with downward leader to provide final channel to earth•Not often seen, but frequently heard

- -- -

- - --

---

++

++

+ +

Page 7: 2006 PQIG Workshop The Physics of Lightning Michael F. Stringfellow.

2006 PQIG Workshop

Connecting Leaders

Page 8: 2006 PQIG Workshop The Physics of Lightning Michael F. Stringfellow.

2006 PQIG Workshop

Return Stroke

•Large current impulse flows to ground•Large electromagnetic pulse radiated•Leader charge neutralized

Page 9: 2006 PQIG Workshop The Physics of Lightning Michael F. Stringfellow.

2006 PQIG Workshop

VHF Radio Picture - First Stroke

Page 10: 2006 PQIG Workshop The Physics of Lightning Michael F. Stringfellow.

2006 PQIG Workshop

Subsequent Strokes

•"Dart" leaders launched from cloud•Follow path of first return stroke•Tap new cloud charges•Cause subsequent return strokes•Often depart from old path

Page 11: 2006 PQIG Workshop The Physics of Lightning Michael F. Stringfellow.

2006 PQIG Workshop

VHF Radio Picture Subsequent Stroke

Page 12: 2006 PQIG Workshop The Physics of Lightning Michael F. Stringfellow.

2006 PQIG Workshop

Video Stills of Multi-Stroke Flash

Page 13: 2006 PQIG Workshop The Physics of Lightning Michael F. Stringfellow.

2006 PQIG Workshop

Multiple Stroke Flashes

•Typically 2-4 strokes per flash•Stroke intervals 5 -100 milliseconds•Reach ground at 1 to 5 points•Severe flashes have >4 strokes•Continuing currents likely

Page 14: 2006 PQIG Workshop The Physics of Lightning Michael F. Stringfellow.

2006 PQIG Workshop

Multiple Ground Channels

•Multiple ground channels are common

• Root branching• Simultaneous leader

branches• Successive strokes

may depart from "main" channel

•Three major channels for every two flashes

Page 15: 2006 PQIG Workshop The Physics of Lightning Michael F. Stringfellow.

2006 PQIG Workshop

Multiple Ground Channels

Page 16: 2006 PQIG Workshop The Physics of Lightning Michael F. Stringfellow.

2006 PQIG Workshop

Currents & Voltages

•Cloud charging current a few amps•Cloud voltages 50 MV to 500 MV•Leader currents 10 A to 1000 A •Return stroke currents 5kA to 500 kA

– Approximately log-normal distribution with 30 kA to 40 kA median

0 50 100 150 200 250 300

Microseconds

0

20

40

60

80

100

120

Kiloamperes

Return Stroke Current

Page 17: 2006 PQIG Workshop The Physics of Lightning Michael F. Stringfellow.

2006 PQIG Workshop

TIE-LINE

2

TRANSMISSION DISTRIBUTIONPRODUCTION

MEDIUMVOLTAGE

EXTRA HIGHVOLTAGE345-765 kV

HIGHVOLTAGE115-230kV

LOWVOLTAGE120-600V

MEDIUMVOLTAGE

24-69kV

PLANTS

POWER INTERCONNECTING

SUBSTATIONS

DISTRIBUTION

SUBSTATIONS

TRANSMISSION

SUBSTATIONS TRANSMISSION

SUBSTATIONS

SMALL INDUSTRIAL

COMMERCIAL

RESIDENTIAL

MEDIUM

INDUSTRIAL

USER

HEAVY

INDUSTRIAL

USER

1

Electricity Production, Transmission & Distribution

Page 18: 2006 PQIG Workshop The Physics of Lightning Michael F. Stringfellow.

2006 PQIG Workshop

Lightning and Overhead Lines

• Direct strikes affect all voltage systems– Problems decrease with insulation level– Flashover when lightning strikes phase conductor– Also back flashover when tower or shield wire struck

• Indirect strikes affect distribution and sub-transmission systems– Induced voltages up to 300 kV

Page 19: 2006 PQIG Workshop The Physics of Lightning Michael F. Stringfellow.

2006 PQIG Workshop

Striking Distance

•Major influences– Height of structure– Charge on lightning

leader– Slenderness of

structure– Random effects

Striking Distance

Capture Radius "Rc"

Charge "Q"Current "I"

Height "H"

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Page 20: 2006 PQIG Workshop The Physics of Lightning Michael F. Stringfellow.

2006 PQIG Workshop

Striking Distance

•Can be inferred from photographs

– Point of last downward branch

– Upward connecting leader path

– Apparent junction

Page 21: 2006 PQIG Workshop The Physics of Lightning Michael F. Stringfellow.

2006 PQIG Workshop

Voltages from Direct Strikes to Overhead Lines

• Stroke to conductor– Conductor has surge impedance of about 400 ohms– Average return stroke current 30 kA– Conductor voltage = 400 x 15,000 V = 6 MV

• Stroke to tower– Tower has footing resistance of 30 ohms– Tower voltage = 30 x 30,000 V = 900 kV

• Shielding and grounding provide effective protection– Especially for higher voltage systems

Page 22: 2006 PQIG Workshop The Physics of Lightning Michael F. Stringfellow.

2006 PQIG Workshop

Transmission Lines & Lightning

•Characteristics– Shielded construction – High insulation levels– Good tower grounding– Effective protection

• Well coordinated fast switchgear

•Result– Excellent lightning

performance– Permanent damage rare– Few flashovers quickly cleared

by protection

Page 23: 2006 PQIG Workshop The Physics of Lightning Michael F. Stringfellow.

2006 PQIG Workshop

Shielding Effectiveness

Page 24: 2006 PQIG Workshop The Physics of Lightning Michael F. Stringfellow.

2006 PQIG Workshop

Shielding Failure

•Likely low current strokes

– Less leader charge

– Smaller striking distance

– Flashover less probable

Page 25: 2006 PQIG Workshop The Physics of Lightning Michael F. Stringfellow.

2006 PQIG Workshop

Distribution Lines & Lightning

•Characteristics– Unshielded construction – Low insulation levels– Poor pole grounding– Less effective protection

• Slower switchgear, autoreclosers and fuses

•Result– Poor lightning performance– Permanent damage common– Many flashovers cleared

• Some may take several shots– Nuisance fuse blowing– Many sags and short-duration

outages

Page 26: 2006 PQIG Workshop The Physics of Lightning Michael F. Stringfellow.

2006 PQIG Workshop

Voltages from Indirect Lightning Strikes

1

10

100

1000

10 100 1000

Induced Voltage kV

Nu

mb

er

pe

r Y

ea

r

Page 27: 2006 PQIG Workshop The Physics of Lightning Michael F. Stringfellow.

2006 PQIG Workshop

Induced Voltage Flashover

Page 28: 2006 PQIG Workshop The Physics of Lightning Michael F. Stringfellow.

2006 PQIG Workshop

Lightning Transients on AC Power System

Page 29: 2006 PQIG Workshop The Physics of Lightning Michael F. Stringfellow.

2006 PQIG Workshop

Lightning Transients on AC Power System

Page 30: 2006 PQIG Workshop The Physics of Lightning Michael F. Stringfellow.

2006 PQIG Workshop

Some Power System Lightning Problems

Multi-stroke flashes can stress switchgear– Transients occur when open

Multi-channel flashes can defeat system protection– Simultaneous faults occur on different parts of circuit

Frequent strikes in severe storm can overwhelm protection

“Weak-link” structures will flash over frequently– May limit line performance

Page 31: 2006 PQIG Workshop The Physics of Lightning Michael F. Stringfellow.

2006 PQIG Workshop

Lightning Tracking

•Radio location used to locate lightning

– Real time• Storm warning• Allocation of resources

– Archival data• Lightning flash density• Fault investigations

Page 32: 2006 PQIG Workshop The Physics of Lightning Michael F. Stringfellow.

2006 PQIG Workshop

Lightning Incident Investigation

Page 33: 2006 PQIG Workshop The Physics of Lightning Michael F. Stringfellow.

2006 PQIG Workshop

US Flash Density

Page 34: 2006 PQIG Workshop The Physics of Lightning Michael F. Stringfellow.

2006 PQIG Workshop

Ground Flash Density

• Highest in southeast & Gulf coast USA• Tampa bay 60 per square mile per year• Houston 40 per square mile per year

• Lower as you move north and west• Washington & Alaska < 0.1 per square mile

per year• Phoenix area ~10 per square mile per year

• Highly variable from year to year • Lightning “hot spots” or “lightning nests”

Page 35: 2006 PQIG Workshop The Physics of Lightning Michael F. Stringfellow.

2006 PQIG Workshop

Lightning Hot Spots

• Local areas of high lightning incidence• Appear over several years’ recording

• Important to ignore short-term random variations• May reflect surface features that steer or promote storms

• Mountains & rivers• Cities• Industries

• May be useful for line performance improvements• Shielding• Arresters • Enhanced grounding

Page 36: 2006 PQIG Workshop The Physics of Lightning Michael F. Stringfellow.

2006 PQIG Workshop

Phoenix Lightning Ground Flash Density

Page 37: 2006 PQIG Workshop The Physics of Lightning Michael F. Stringfellow.

2006 PQIG Workshop

Summary

• Overhead transmission lines are resistant to lightning– Shielded, grounded, high insulation levels– EHV systems are almost immune

• Electricity distribution systems are vulnerable– Unshielded, poorly grounded, low insulation levels– Some newly discovered challenges from multi-

channel flashes• Lightning location systems have many benefits

– Real-time tracking– Archival flash density