How to go to your page This eBook contains two volumes. In the printed version of the book, each volume is page-numbered separately. To avoid duplicate page numbers in the electronic version, we have inserted a volume number before the page number, separated by a hyphen. For example, to go to page 5 of Volume 1, type 1-5 in the "page #" box at the top of the screen and click "Go." To go to page 5 of Volume 2, type 2-5… and so forth. ENCYCLOPEDIA OF weather and climate Revised Edition Volume I A–o michael allaby 0i-xviii_WC_fm.indd i 5/17/07 11:51:02 AM ENCYCLOPEDIA OF WEATHER AND CLIMATE, Revised Edition Copyright © 2007, 2002 by Michael Allaby All rights reserved. No part of this book may be reproduced or utilized in any form or by any means, electronic or mechanical, including photocopying, recording, or by any information storage or retrieval systems, without permission in writing from the publisher. For information contact: Facts On File, Inc. An Imprint of Infobase Publishing 132 West 31st Street New York NY 10001 ISBN-10: 0-8160-6350-8 (set) ISBN-13: 978-0-8160-6350-5 (set) Library of Congress Cataloging-in-Publication Data Allaby, Michael. Encyclopedia of weather and climate / [Michael Allaby].—Rev. ed. p. cm. Includes bibliographical references and index. ISBN 0-8160-6350-8 (set)— ISBN 0-8160-6348-6 (v.1)—ISBN 0-8160-6349-4 (v. 2) 1. Meteorology— Encyclopedias. 2. Climatology—Encyclopedias. I. Title. QC854.A452007 551.603—dc22 2006018295 Facts On File books are available at special discounts when purchased in bulk quantities for businesses, associations, institutions, or sales promotions. Please call our Special Sales Department in New York at (212) 967-8800 or (800) 322-8755. You can find Facts On File on the World Wide Web at http://www.factsonfile.com Text design by Joan M. McEvoy Cover design by Salvatore Luongo Illustrations by Richard Garratt Photo research by Tobi Zausner, Ph.D. Printed in the United States of America VB Hermitage 10 9 8 7 6 5 4 3 2 1 This book is printed on acid-free paper. 0i-xviii_WC_fm.indd ii 5/17/07 11:51:03 AM C ONTENTS Acknowledgments v Introduction vi Abbreviations and Acronyms ix Entries A–O 1 APPENDIXES I. Biographical Entries 573 II. Tropical Cyclones and Tropical Storms 655 III. Chronology of Tornadoes 669 IV. Laws, Regulations, and International Agreements 673 V. The Geologic Timescale 675 iii 0i-xviii_WC_fm.indd iii 5/17/07 11:51:03 AM VI. Ocean Currents 677 VII. Pliocene, Pleistocene, and Holocene Glacials and Interglacials 691 VIII. SI units and conversions 693 IX. Chronology of Disasters 695 X. Chronology of Discoveries 703 Bibliography and Further Reading 709 Web Sites 711 Index I-1 0i-xviii_WC_fm.indd iv 5/17/07 11:51:03 AM A CKNOWLEDGMENTS My friend Richard Garratt drew all of the maps, diagrams, and other line drawings in this encyclopedia. Richard and I have collaborated on many projects, spanning more years than either of us cares to count. He has a genius for translating my crude sketches into accurate and attractive illus- trations. As always, I am deeply grateful to him. There were not many photographs in the first edition of the encyclo- pedia, but we decided to include them in this edition. I drew up a long list of topics I thought might benefit from a photograph and sent the list to Tobi Zausner. With great perseverance and unfailing good humor she gathered together the pictures you will see here. Without Tobi’s help this would be a less informative book than it is, and one less pleasing to the eye. Finally, I must thank my friends at Facts On File. In particular, I would like to thank my editor, Frank K. Darmstadt, for his patience, wisdom, and the kindly interest he always shows in the well-being of his author and for the polite interest he shows in the current loca- tion of the text he was supposed to have received weeks or months ago. Appreciation also goes to his assistant, Alana Braithwaite, for going through this huge manuscript and getting all of its elements in order for production to take over. This work is not a compilation of entries written by contributors. I wrote all of the entries myself. The consequence is that any mistakes that have escaped Frank’s eagle eye are entirely my own work. So are the facts I got right, of course. v 0i-xviii_WC_fm.indd v 5/17/07 11:51:03 AM I NTRODUCTION Everyone has an interest in the weather, and in recent years that interest has intensified. Climates always change over long periods. The weather the world experiences today is different from that of the Little Ice Age of the 17th century and of the Middle Ages, when the climate was warm and England was a major wine producer. Today, though, there are fears that the climate may be changing faster than it has done for thousands of years and that the gases released into the air from cars, factories, domestic fires, power stations, farming, and forest clearance may be accelerating that change. This concern is now driving climatic research. The climate of a place or of the world is the average weather that it experiences over a long period. On a shorter timescale, the day-to-day weather affects everyone. Those who set off for school or work without a coat or umbrella may get a soaking if they forget to check before leav- ing home whether it is raining. In winter, when snow and ice are likely, drivers should check before setting off whether the roads are safe and, if they are, whether conditions are likely to deteriorate. Misjudgments can be serious. Snowfalls can make roads impassable, marooning people in their cars where the low temperature can kill. Some people need to know about the coming weather in more detail. Fishermen must know whether it will be safe for them to put to sea. Sailors of all kinds need to know whether they are sailing into a severe storm and, if so, how to avoid it. Pilots need to know the speed and direction of the winds along the routes they plan to fly. These determine the time the journey will take and the amount of fuel the aircraft will consume. Extreme weather such as tornadoes, tropical cyclones, and floods can cause widespread devastation. Lives can be saved and damage to prop- erty minimized if communities receive adequate warning and respond appropriately. The warning may be broadcast on behalf of the govern- ment by a radio or television station, but it is based on information sup- plied by meteorologists—the scientists who study, monitor, and forecast the weather. There are also less immediate ways in which the weather affects people. Fine growing weather across the farmlands of the nation, with rain when it is needed and sunshine to ripen the crops, produces heavy crop yields. Food is abundant, and when a commodity is abundant its vi 0i-xviii_WC_fm.indd vi 5/17/07 11:51:03 AM Introduction vii price falls. So fine weather can make food cheaper. In the same way, bad weather can lead to low yields and higher prices. Changes in food prices may make the difference between relative prosperity and hardship for the poorest members of society, and in some parts of the world bad weather may lead to famine, in which people die. Mild winters reduce heating bills. People do not need so much ener- gy to warm their homes as they do when the winter is hard. This makes a difference to living costs, and it also has environmental consequences. Burning fossil fuels—coal, oil, or gas—to generate electrical power, or directly for space heating, water heating, and cooking, releases by-prod- ucts of combustion into the air. Some of these, such as sulfur dioxide, carbon monoxide, and unburned hydrocarbons, cause pollution. My own interest in weather and climate began many years ago. For a short time I was a military pilot, so I was compelled to observe the weather and to respect it. I learned then that bad weather can kill and that it pays to listen to the weather forecast. More recently, my inter- est has developed from my studies of the environmental sciences. These include the atmospheric sciences of climatology and meteorology as well as the historical disciplines such as paleoclimatology, which is the study of the climates of the distant past. Several years have passed since the previous edition of the Encyclopedia of Weather and Climate was published. Research in the atmospheric sciences is intense, and so much has happened during those years that a new edition seemed advisable. This edition contains a num- ber of new entries, but almost all of the entries from the earlier edition have been revised. Some have been expanded and others modified to take account of recent discoveries about the atmosphere and the way it works. The preparation of a new edition also made it possible to alter the overall structure of the encyclopedia. Many of the shorter entries in the earlier edition have been assembled into longer essays in this edition. Some short entries remain, but this edition contains a smaller number of much longer essays that incorporate all the information from the earlier edition—and often more. Certain categories of entry have been removed altogether from the main body of the encyclopedia and are contained in 10 appendixes. The appendixes contain biographical notes on more than 120 individual sci- entists, as well as lists of the most severe tropical cyclones and tropi- cal storms, tornadoes, weather disasters, and milestones in atmospheric research. The principal ocean currents are also listed alphabetically and described in an appendix. I hope that placing this material in appendixes makes it more easily accessible. The main body of the encyclopedia contains entries describing pro- cesses such as cloud formation, atmospheric phenomena such as rain- bows, and some of the techniques and instruments that are used to study the atmosphere, as well as the units of measurement that scientists use. They also explain the classification systems that are used for climate types, winds, and clouds. The weather we experience is local. It may be raining on one side of a hill and fine on the other side. This means that from time to time 0i-xviii_WC_fm.indd vii 5/17/07 11:51:03 AM viii Introduction many places experience weather conditions different from those in the surrounding region, and the local conditions usually have local names. Winds, in particular, acquire local names. The chinook, Santa Ana, mis- tral, harmattan, bora, and sirocco are just a few of the local names for winds that people in certain places welcome or dread. The encyclope- dia lists some of these, in entries on local weather and local winds, and explains each type and where it occurs. Before there were weather stations, orbiting satellites, and power- ful computers to produce weather forecasts, people had to rely on their experience and the signs they could read, or thought they could read, in the sky and in the natural world around them. Over centuries these expe- riences accumulated as weather lore, comprising sayings, rhymes, and references to clouds, plants, and animals. Some of these are also included here, in an entry on weather lore. Small capital letters (like this) used within entries act as cross-refer- ences, indicating terms for which there are full entries. Items for further reading and relevant Web sites are listed at the end of the entries to which they relate. They are also listed at the end of the encyclopedia. Finally, a note on the units of measurement used here. Many scientif- ic disciplines use special units to describe quantities that are relevant only within those disciplines. Atmospheric chemists, for example, use Dobson units to measure the concentration of atmospheric gases, especially of ozone. Apart from such specialist units, all scientists work in SI units. SI stands for Système International d’Unités (International System of Units). The meaning of individual units (including Dobson units) is explained in the entry “units of measurement”; SI units are listed with their abbrevia- tions and, where appropriate, conversions to customary units. Meteorologists measure air pressure in pascals, but weather forecast- ers often use the older unit, the millibar (1 millibar = 100 pascals). Temperatures are reported in degrees Celsius (°C) or in kelvins (K), depending on the context. In this encyclopedia, temperatures are given in degrees Fahrenheit (°F) with °C in parentheses. Rainfall is always reported in millimeters and never in centimeters. There are two reasons for this. The first is to avoid decimal fractions so far as is possible by using a small unit. The second is to avoid the confu- sion that might occur if two units were used, one of which is 10 times bigger than the other. In all entries in this Encyclopedia of Weather and Climate, Revised Edition, rainfall is given in inches with millimeters in parenthesis. I hope you enjoy wending your way through the highways and byways of atmospheric science as you explore the processes that generate our weather. Writing the encyclopedia was fun. I hope it is fun to use. —Michael Allaby Tighnabruaich Argyll, Scotland www.michaelallaby.com 0i-xviii_WC_fm.indd viii 5/17/07 11:51:03 AM
Description: