WHAT WOULD HAPPEN IF LIGHTNING WERE ELIMINATED? by MARTIN A. UMAN ORIGINALLY PUBLISHED IN

Similar documents
5/26/2010. Hailstone Formation and Growth Lightning Stroke Downburst Formation, Structure, and Type

Chapter 21. Lightning Facts. Lightning Facts 4/12/17. Lightning

Chapter 19, Electricity Physical Science, McDougal-Littell, 2008

Lightning. Electricity and Charge. Primary types of lightning. Primary types of lightning. How do clouds gain a charge?

Dr. Kim D. Coder, Professor of Tree Biology & Health Care, Warnell School, UGA

(part I) Dr. Kim D. Coder. Professor of Tree Biology & Health Care Warnell School, University of Georgia

Energy Stored in Capacitors

A little E&M review. Coulomb s Law Gauss s Law Ohm s Law

ELECTROSTATICS. When two materials rub together the contact between their surfaces may cause: a) the surfaces to become hot and show wear and tear.

Lightning in Florida. Henry E. Fuelberg Department of Meteorology Florida State University

SkyScan EWS-PRO - Manual -

Section 9: Using a Charged Electroscope to Determine the Charge on Another Object. Examples:

THE VISUAL IDENTIFICATION OF LIGHTNING-

LECTURE #15: Thunderstorms & Lightning Hazards

1.64 Static Electricity and Static Discharge

Opening. Monster Guard. Teacher s Guide

TUBES FORMED BY LIGHTNING

III. Section 3.3 Vertical air motion can cause severe storms

National Weather Service Morristown, Tennessee Lightning and Weather - What Every Trail Rider Needs to Know to Protect Themselves

E2 - Electric Field. Electrostatic & gravitational force. Electric Field. act at a distance, no direct push or pull

6.7 Thunderstorm Electrification

Today s lecture. Charge separation in clouds Lightning and thunder

& Locations. Dr. Kim D. Coder, Professor of Tree Biology & Health Care, Warnell School, UGA

3 Severe Weather. Critical Thinking

Electric Forces and Electric Fields

Electric Charge. Physics 4B. Atomic Structure

Physics 196 Final Test Point

iclicker A device has a charge q=10 nc and a potential V=100V, what s its capacitance? A: 0.1 nf B: 1nF C: 10nF D: F E: 1F

iclicker A metal ball of radius R has a charge q. Charge is changed q -> - 2q. How does it s capacitance changed?

Current Electricity refers to

, times the dielectric constant of the material, k d. . With these definitions, Eq. 1 can be written as:

Electric Potential. Chapter 23. PowerPoint Lectures for University Physics, Twelfth Edition Hugh D. Young and Roger A. Freedman

The Atmosphere Made up of mainly two gases: Nitrogen 78% Oxygen 21% Trace Gases 1%

Thunderstorm. Thunderstorms result from the rapid upward movement of warm, moist air.

Notes on Electricity (Circuits)

THUNDERSTORMS. Convective heavy rain accompanied by lightning and thunder. Ahrens

Coimisiún na Scrúduithe Stáit State Examinations Commission

Chapter Assignment Solutions

Recap: Electric Field Lines Positive Charge: field lines outwards direction Negative Charge: converge F + In both cases density

Conductors and Electric Fields in Static Equilibrium

Lightning Parameters for Engineering Applications: Recent Updates and Outlook

Concurrent Upward Lightning Flashes from Two Towers

Weather - is the state of the atmosphere at a specific time & place

ELECTRICITY. Electric Circuit. What do you already know about it? Do Smarty Demo 5/30/2010. Electric Current. Voltage? Resistance? Current?

Electrostatics. Physics 10. Atomic Structure

REFERENCES TO LIGHTNING IN THE HOLY BIBLE

Observation of Cloud-to-Ground Lightning Channels with High-Speed Video Camera

Electric Fields 05/16/2008. Lecture 17 1

Earth Science Weather and Climate Reading Comprehension. Weather and Climate

Electric Fields Practice Multiple Choice

Key Concept Weather results from the movement of air masses that differ in temperature and humidity.

Thunderstorms form from rising moist air.

Name Date Time to Complete

20.1 Air Masses. Weather Patterns and Severe Storms. Four Types of Source Regions. Weather in North America Fronts

L 24 Electricity & Magnetism [2]

Guided Notes: Atmosphere Layers of the Atmosphere

Chapter 2: Capacitors And Dielectrics

Chapter 16 Electrical Energy Capacitance. HW: 1, 2, 3, 5, 7, 12, 13, 17, 21, 25, 27 33, 35, 37a, 43, 45, 49, 51

Jim Witt Long Range Calendar

Guided Notes Weather. Part 2: Meteorology Air Masses Fronts Weather Maps Storms Storm Preparation

The Earth System - Atmosphere III Convection

Electricity MR. BANKS 8 TH GRADE SCIENCE

Electricity. Chapter 21

Electricity Electrostatics Types of materials Charging an Object Van de Graaff Generator

Ideal wires, Ideal device models, Ideal circuits. Ideal models for circuit elements Wires

Thunderstorms. Stages in the development of a thunderstorm

Chapter 3 Static and Current Electricity

Let s Think for a Second

THUNDERSTORMS Brett Ewing October, 2003

Weather Elements (air masses, fronts & storms)

High speed video observations of a lightning stepped leader

THE ESSENCE OF... HAO~ Edward N. Lorenz UNIVERSITY OF WASHINGTON PRESS. Seattle

Unit 4 Review Guide: Weather

Lightning. lightning: an electrical discharge in the atmosphere. Electricity. Lightning, Thunder and Tornados PHYS 189. Electricity.

Notes on Electricity (Circuits)

Weather. All photos, graphics, and text copyright 2007 Kris Light

9/13/2012. Chapter 4. Atmospheric Moisture, Condensation, and Clouds.

Chapter 4. Atmospheric Moisture, Condensation, and Clouds. 9/13/2012

Chapter 21 Electric Current and Circuits

Weather Systems III: Thunderstorms and Twisters

Consider a point P on the line joining the two charges, as shown in the given figure.

Lightning Interception. Non conventional lightning protection systems

Electric Force and Charges. Conceptual Physics 11 th Edition. Electric Force and Charges

7. Static Electricity and Capacitance

Weather: Air Patterns

The Mysteries of Lightning Joseph R. Dwyer Department of Physics and Space Science Center, University of New Hampshire

Questions Q1. A battery sends a current through a metal wire. ) in the box next to your answer. (a) (i) Complete the sentence by putting a cross (

2. Electrical forces cancel out, leaving weaker gravity predominant.

UNIT V: Electricity and Magnetism Chapters 32-37

HOW VOLTAGE, CURRENT, AND RESISTANCE RELATE

Section 3. Series and Parallel Circuits: Lighten Up. What Do You See? What Do You Think? Investigate

Satellite communications and the environment of space

Lecture Notes (Applications Of Electric Fields)

Lecture Power Points. Chapter 16 Physics: Principles with Applications, 6 th edition Giancoli

Air Mass Thunderstorms. Air Mass Thunderstorms. Air Mass Thunderstorms. Lecture 26 Air Mass Thunderstorms and Lightning

What are the two types of current? The two types of current are direct current and alternating current.

Buoyancy and Archimedes Principle

Lightning Protection Of Wind Turbines

AP Physics Study Guide Chapter 17 Electric Potential and Energy Name. Circle the vector quantities below and underline the scalar quantities below

Lecture Outlines. Chapter 28. Astronomy Today 8th Edition Chaisson/McMillan Pearson Education, Inc.

Transcription:

WHAT WOULD HAPPEN IF LIGHTNING WERE ELIMINATED? by MARTIN A. UMAN ORIGINALLY PUBLISHED IN ALL ABOUT LIGHTNING DOVER PUBLICATIONS, NEW YORK, 1986

ORIGINALLY PUBLISHED IN ALL ABOUT LIGHTNING DOVER PUBLICATIONS, NEW YORK, 1986 WHAT WOULD HAPPEN IF LIGHTNING WERE ELIMINATED? by MARTIN A. UMAN First, it is appropriate to point out that it may well have been lightning in the primordial soup covering the earth several billion years ago that produced the complex molecules from which life eventually evolved. Laboratory experiments have shown that electrical discharges in what is believed to be the constituents of the primordial atmosphere can create the necessary molecules. Thus, we may be indebted to lightning for the presence of life on earth. Still, lightning is primarily troublesome rather than helpful, as the contents of this book attest, and except for some of the benefits mentioned in the previous chapter it might seem advantageous to eliminate it altogether. Exactly what would hap-

Figure 18.1: Thunderstorms act as batteries to keep the earth charged negatively and the atmosphere charged positively. Atmospheric electrical currents flow downward in fine weather and upward in thunderstorms. Thunderstorms deliver charge to the earth by lightning, rain, and corona discharges. pen if lightning were eliminated is not known, but clearly the electrical balance of the atmosphere would have to change as we shall see in the following paragraphs. If and how the change in electrical balance would change the weather is not known. Prudence, however, would dictate extreme caution in tampering with lightning. The electrical resistivity of the atmosphere decreases with height. From the point of view of atmospheric electricity, the resistivity is sufficiently low at an altitude of about 30 miles that the voltage does not vary much above that point. The region beginning at about 30 miles and extending upward is called the electrosphere. (The ionosphere, which reflects lightning

Figure 18.2: Lightning over Lake Chiem in Bavaria, Germany. (Courtesy, Agfa- Gavaert AG) radio waves downward, begins, as noted in Chapter 17, at about 40 miles and is even a better conductor than the bottom of the electrosphere.) The voltage between the earth and the electrosphere in regions of fine weather is about 300,000 volts. To maintain this voltage the earth has a negative charge of about a million coulombs on its surface and an equal net positive charge is distributed throughout the atmosphere. Measurements have shown that the negative charge on the earth remains roughly constant with time. At first glance, this fact is difficult to understand since the charge on the earth is continuously leaking off into the conducting atmosphere. In fact, calculations show that, if the earth s charge were not being continuously re-supplied, the charge on the earth would disappear in less than an hour.

Figure 18.3: Lightning over the Arizona desert. (Courtesy, J. Rodney Hastings, University of Arizona) The earth is recharged by thunderstorms. Fig. 18.1 shows how the electrical balance of the atmosphere is maintained. Thunderstorms deliver a net negative charge to the earth as a result of the sum of the effects of the following processes: (1) negative charge carried from cloud to earth by lightning, (2) positive charge carried from cloud to ground by rain, and (3) positive charge carried upward (the equivalent of negative charge carried downward) through the air beneath and above a thunderstorm, the source of the positive charge being corona discharge off grass, trees, and other objects with sharp points on the ground beneath the thunderstorms. The total current flowing beneath all thunderstorms in progress throughout the world at any given time is thought to be about 2,000 amps, and is in

Figure 18.4: A lightning flash exhibiting multiple ground points and the ribbon effect discussed in Chapter 16. (Courtesy, George Marcek, Catalina High School, Tuscon) such a direction as to charge the earth negatively. An approximately equal and opposite current flows in regions of fine weather. The result is that the net negative charge on the earth and the equal and opposite net positive charge in the atmosphere remain approximately constant. Finally, if all lightning were eliminated, we earthly viewers would be deprived of one of the most spectacular visual displays that Nature has to offer. In its variety and brilliance lightning puts man-made fireworks to shame, as evidenced by Figs.

Figure 18.5: Lightning initiated by an upward-moving leader from a tower on Mt. San Salvatore near Lugano, Switzerland. Photographs of other discharges to the tower are shown in Fig. 6.1a, b. (Courtesy, Richard E. Orville, State University of New York at Albany) 18.2 to 18.5. Watching lightning is fun; one of the aims of this book has been to make it more so. Many confirmed lightning watchers even enjoy listening to the variety of sounds that comprise thunder. REFERENCES The details of and references to the bulk of the material found in this chapter are to be found in Atmospheric Electricity, J. A. Chalmers, 2nd Edition, Pergamon Press, New York, 1967, pp. 33-35, 292-308.

THE EVENT PETRIFIED LIGHTNING FROM CENTRAL FLORIDA A PROJECT BY ALLAN MCCOLLUM CONTEMPORARY ART MUSEUM UNIVERSITY OF SOUTH FLORIDA MUSEUM OF SCIENCE AND INDUSTRY TAMPA, FLORIDA