Before the end of the nineteenth century, a weatherman in Australia

named Clement Wragge had begun giving girls' names to tropical storms.

Down in that part of the Southern Hemisphere, hurricanes are called

willy-willies. They come from the tropics on a southwest course and turn

to the south and southeast on approaching or passing Australia. Their

winds spiral inward around the center in a clockwise direction--the

opposite of the turning motion of our hurricanes.

Wragge was the government meteorologist in Queensland, and later ran a

weather bureau of his own in Brisbane. A tall, thin, bewhiskered man who

stammered, he was known all over Australia as a lecturer on weather and

similar subjects. Australians of that time said that, as likely as not,

when due to talk about big winds, he would arrive at the lecture hall

with "too many sheets out" and fail to keep on his feet during the

lecture. Though his name was Clement, he was better known in Australia

as "Inclement."

Storms which did not come from the tropics were called by men's names.

Generally, Wragge called them after politicians who had earned his

disfavor, but for some reason he used girls' names for the

willy-willies. As an illustration for his weather journal called

"WRAGGE," he had a weather map for February 2, 1898, with a willy-willy

named "Eline." He predicted nasty weather from a disturbance named

"Hackenbush."

E. B. Buxton, a meteorologist for Pan American Airways, went to the

South Pacific in the late thirties and, after hearing about Wragge and

his names for willy-willies, adopted the idea for his charts. He

recalled particularly using the name "Chloe" for hurricanes.

With few exceptions, the hurricanes of the twentieth century went

unnamed in the United States until 1951, although some were referred to

in terms of place and date; for instance, the "New England Hurricane of

1938." Unofficially, a few had names of people. In 1949, while President

Truman was in Miami addressing the Veterans of Foreign Wars, the first

hurricane of the season was called "Harry," and a little later a bigger

one which the newsmen said had greater authority struck southern Florida

and it was called "Hurricane Bess."

In sending out advices and warnings of West Indian storms, it was not

considered necessary to have names, as it was seldom that more than one

was in existence at the same time. In 1944, when aircraft reconnaissance

began, it became customary to get reports by radio-telephone and voice

was used increasingly in other ways by the hurricane hunters. But this

gave no particular trouble until September, 1950, when there were three

hurricanes in progress at the same time.

Two were in the Atlantic, one north of Bermuda and the other north of

Puerto Rico. The third appeared in the eastern Gulf of Mexico. When

aircraft were dispatched into these storms and began reporting, there

was increasing confusion. Other communications and public advices became

mixed and there was much uncertainty as to which storm was meant. Use of

letters of the alphabet to identify them was no help, for letters B, C,

D, E, and G sound much alike by radio-telephone; also A, J, and H.

Numbers were no better because weather reports are sent by numbers and

the advisories issued on each storm are numbered, so that the number 3

could be the number of the storm, the number of the advice, an element

of the weather, the hour, etc.

The agencies involved in weather and communications in connection with

hurricanes met early in 1951 and decided to identify storms by the

phonetic alphabet, which gave Able for A, Baker for B, Charlie for C,

etc., in accordance with the following table:

Able

Baker

Charlie

Dog

Easy

Fox

George

How

Item

Jig

King

Love

Mike

Nan

Oboe

Peter

Queen

Roger

Sugar

Tare

Uncle

Victor

William

Xray

Yoke

Zebra

In the 1951 season, this worked very well in the communications and the

public began to speak of hurricanes by these names. At the start of the

1952 season, the agencies began to use the same list of names, starting

with Able for the first storm, but soon ran into difficulty. A new

international alphabet had been introduced as follows:

Alfa

Bravo

Coca

Delta

Echo

Foxtrot

Golf

Hotel

India

Joliet

Kilo

Lima

Metro

Nectar

Oscar

Papa

Quebec

Romeo

Sierra

Tango

Union

Victor

Whiskey

Extra

Yankee

Zulu

Some of the agencies had begun using the new alphabet in their

communications, while others stuck to the old one. So the third storm of

the season was "Charlie" part of the time and the rest of the time some

wanted to call it "Coca." At the end of the season there was no

agreement as to which phonetic alphabet should be used and there was

criticism for having continued an alphabet which was obsolete

internationally.

After a long discussion, military members of the conference suggested

adoption of girls' names, which had been used successfully for typhoons

in the Pacific for several years. Just how this practice originated is

not known, but it was thought by some persons to have come from the book

_Storm_, by George R. Stewart, which was published in 1941. In this book

a fictitious Pacific storm is traced to the United States and its

effects on the people are narrated in the style of a novel. A young

weatherman at San Francisco, according to the story, called the storm

Maria. Also there was Wragge's use of girls' names for willy-willies in

Australia and Pan American Airway's practice in connection with

hurricanes as early as 1938. At any rate, with these Pacific precedents,

the weathermen and hurricane hunters adopted the following list for 1953

for hurricanes in the Atlantic, Caribbean and Gulf of Mexico:

Alice

Barbara

Carol

Dolly

Edna

Florence

Gilda

Hazel

Irene

Jill

Katherine

Lucy

Mabel

Norma

Orpha

Patsy

Queen

Rachel

Susie

Tina

Una

Vicky

Wallis

This list worked perfectly in 1953; the public was pleased; the

communicators were happy about it; the newspapers thought it was

colorful; and use of the same names began to spread in Canada and some

of the countries to the southward. The same list was adopted with

enthusiasm for the 1954 season.

In 1954, Alice and Barbara were minor hurricanes in the Gulf of Mexico,

although Alice broke up in tremendous rains in the upper watershed of

the Rio Grande, after moving inland over Mexico. There were floods which

broke records for all time as the water moved down the river. The third

storm, Carol, started a controversy in the press and many letters were

written to the editors and to the Weather Bureau, some favoring the

scheme or trying to get a little fun out of it, but most of them finding

objections of one kind or another. It was almost impossible to change in

the middle of the season, even if the hurricane hunters had wanted to,

so it was continued during 1954 and each new hurricane aroused further

comment. Later Hazel came along about the middle of October, a very

severe hurricane from the Caribbean Sea. It turned northward between

Cuba and Haiti and caused terrible damage and much loss of life. Later

it struck the coast of the Carolinas and crossed the eastern states

northward to New York. Loss of life in the eastern states was variously

estimated from fifty to eighty, and the damage to property, especially

from falling trees, was enormous. There was another flood of complaints,

this time about the name Hazel.

Before the argument was ended it threatened to be almost as stormy as

some of the smaller hurricanes so named. Early in 1955 the Weather

Bureau had a meeting with the Air Force, Navy and others interested in

deciding the question. By that time the opinions received by mail were

overwhelmingly in favor of continuing girls' names. In the meantime,

there had been a surprise. A storm having some of the characteristics of

a hurricane was sighted in the Caribbean Sea in January and, in the

absence of a decision on names to be used in 1955, it was called Alice

from the 1954 list. Later, the names for others in 1955 were decided as

follows:

Brenda

Connie

Diane

Edith

Flora

Gladys

Hilda

Ione

Janet

Katie

Linda

Martha

Nellie

Orva

Peggy

Queena

Rosa

Stella

Trudy

Ursa

Verna

Wilma

Xenia

Yvonne

Zelda

_17._ THE GEARS AND GUTS OF THE GIANT

"_he that wrestles with us strengthens our nerves and sharpens our

skill_"

--Burke

All through this book we have talked about hurricane hunters. By now it

is clear that the crew on the plane that goes into the storm at the risk

of destruction of the craft and death to the men is not really "hunting"

a hurricane. It is the exception rather than the rule when they discover

a tropical storm. The first hint comes from some distant island or a

ship in the gusty wind circle where the sea and the sky reveal ominous

signs of trouble. Somewhere in a busy weather office a large outline map

is being covered with figures and symbols. Long, curving lines across a

panorama of weather take shape as the radios vibrate and the

teletypewriters rattle with the international language of

weathermen--the most co-operative people in the world's family of

nations.

Hurricane hunting is done on these maps. Day after day, without any

fanfare, the weathermen search the reports spread across this almost

boundless region where hundreds of tropical storms could be in progress

if nature chose to operate in such an eerie fashion. Even the

experienced observers on islands and the alert officers on shipboard

might not see the real implications in the weather messages they

prepare. In the enormous reaches of the belt of trade winds, where the

tremendous energy of the sun's heat and the irresistible force of earth

rotation dictate that the winds shall blow as steady breezes from the

northeast, somebody might put in his report, for example, that there was

a light wind coming from the southwest. That fact alone would be enough.

In season, the weathermen would know, almost with certainty, that there

was a tropical storm in the area.

There are many things to watch for, in the array of elements at the

surface, in the upper air, the clouds, sea swells, change of the

barometer, faint earth tremors. A hint from this scattering of messages

in the vast hurricane region starts the action. And the planes go out to

investigate.

This is an extraordinary procedure. Looking at it as an outgrowth of the

insistent demands of citizens along the coasts in the hurricane region

for warnings of these storms, as the population increased and property

losses mounted, it seems that the flight of planes into these monstrous

winds is justified only until a safer method can be found. All other

aircraft are flown out of the threatened areas, obviously because the

winds are destructive to planes on the ground. The lives of men and the

safety of the plane in the air should not run a risk of being sacrificed

if it can be avoided. Of course, it is argued by some men that there is

a possibility that a method may be discovered to control hurricanes by

the use of chemicals or some other plan requiring planes to fly into the

centers. And it is true, also, that for the time being at least there is

certain information that can be obtained in no other way.

At the end of World War II, there was a grave requirement for more

information about hurricanes. Little was known except in theory about

their causes, maintenance, or the forces which determine their rate and

direction of travel. Since that time, literally thousands of flights

have been made into hurricanes and typhoons. Scientists have studied the

detailed records of these many penetrations.

We have learned a great deal in these years but by no means enough.

Herbert Riehl, a professor of meteorology at Chicago University, has

examined as large quantities of the data as any man. Recently he said,

"Our knowledge regarding the wind distribution within tropical storms

and the dynamical laws that guide the air from the outskirts to the

center of the cyclone is so deficient as to be deplorable."

From the scientific point of view, remarks of this kind are fully

justified, but progress in the issuance of warnings is quite another

matter. Hurricane prediction for the present and the near future is an

art and not a science. Very great progress has been made in recent years

in sending out timely warnings. There are figures to show the facts. At

the beginning of this century, a hurricane causing ten million dollars

in property damage was likely to take several hundred lives. Twenty-five

years later, the average was about 160 lives. Ten years later (1936 to

1940 average) the figure had been reduced to about twenty-five and was

steadily going down. After men began flying into hurricanes, the figure

was reduced to four (1946 to 1950). This is astonishing, not only in

showing how the warnings were improving after hunting by air got

started, but also the big gains shortly before that time, especially

after the hurricane teletypewriter circuit was installed around the

coast in 1935. Experience in prediction, on-the-spot operation, and fast

communications are vital.

In fact, the record was so good at the beginning of World War II that

most forecasters despaired of their ability to keep it up. It had

consistently been below ten lives for ten million dollars' damage and

one serious mistake could have raised this rate considerably for several

years. For this reason, as well as many others, the forecasters were

extremely grateful for the information from aircraft.

The main hope for greater savings in the future is that the solution of

some of the mysteries of the hurricane will enable the forecasters to

send out accurate warnings much farther in advance. In such an event, it

will be possible to protect certain kinds of property and crops which

are being destroyed at present. Heavy equipment can be moved and certain

crops can be harvested in season, if plenty of time is available. These

precautions are time-consuming and costly, and the advance warnings must

be accurate in detail. And it will help to make sure that no hurricane

different from its predecessors will come suddenly and catch us off

guard and cause excessive loss of life. Now and then we have one which

is called a "freak."

One thing we have become increasingly sure of and it will stand

repetition. No two hurricanes or typhoons are alike. Scientists may find

some weather element that seems to be necessary to keep the monster

going, and then are frustrated to find that not all tropical storms have

it. If some can do without it, maybe it is not necessary, after all. And

yet all of them fit a certain direful pattern; there is nothing else

that resembles these big storms of the tropics. Like the explosion of an

atom bomb, with its enormous cloud recognized by everyone who sees a

picture of it, the hurricane has well-known features--unlike anything

else--but of such enormous extent that no one can get a bird's-eye view

of the whole. Putting together what we know by radar, upper air

soundings, aircraft penetrations and millions of weather observations in

the low levels, we can draw a sketchy word picture. Looking down from

space, we could see it as a giant octopus with a clear eye in the center

of its body, arms spiraling around and into this body of violent winds

around the eye--all of the monster outlined by the clouds which thrive

as it feeds on heat and moisture. We feel sure of that much.

The birth of the THING has not been explained. There are plenty of times

when all the ingredients are there. Nothing happens. Observation and

theory flourish and swell into confusion. No scientist can say,

"Everything is just right; tomorrow there will be a hurricane."

Why it moves as it does is another grim puzzle. Ordinarily, the great

storm marches along with the air stream in which it is embedded,

changing its path with the contours of the vast pressure areas which

outline the circulation of the atmosphere, but too often it suddenly

changes its mind, or whatever controls it, or shifts gears, and comes to

a halt, or describes a loop or a hairpin turn. Nobody can see these

queer movements ahead of time. Going out there in an airplane to look

the situation over does not help in this respect. It is a vital aid in

keeping track of the THING and protecting life and property, but it ends

there.

Where does all the air go? When the big storm begins out there over the

ocean, air starts spiraling inward and the pressure falls, showing that

the total amount of air above the sea to the top of the atmosphere is

lessening, even as it pours inward at the bottom. For a hundred years

scientists argued that it must flow outward at the top, that at some

upper level the inflow of air ceases and above that there must be a

powerful reversal of the circulation. Here again we have frustration.

Going up with one of the investigators, we get the facts. Strangely

enough, this is one of the men who want to get into hurricanes, who come

down to the coast to look, and who finally "thumb a ride" with the

airmen into the big winds. A brief of his story will illustrate.

This story begins with the big Gulf hurricane of 1919. It came from the

Atlantic east of the Windward Islands, moved slowly to the northward of

Puerto Rico and Haiti and thence to the central Bahamas, a fairly large

storm threatening the Atlantic seaboard. Then it took an unusual path,

generally westward, with increasing fury. It was a powerful storm as its

central winds ravaged the Florida Keys and took a westward course across

the Gulf. It happened shortly after World War I and there was little

shipping in the Gulf. The slow-moving hurricane, now a full-fledged

tropical giant, dawdled in the Gulf and was lost; that is, lost as much

as a monster of its dimensions can be, but its winds were felt all

around the Gulf Coast and its waves pounded the beaches as it spent four

days out there without disclosing the location or motion of its calm

center.

Warnings flew all around the coast and the week dragged to an end with

the people extremely tired of worrying about it and the weathermen worn

out with continuous duty. Saturday night came and the center seemed to

be no nearer one part of the coast than another. Late at night, an

annoying thing happened. It was customary in those days for the

forecaster, in sending a series of messages from Washington, to stop

them at midnight and begin again early the next morning. It was the rule

that no reports came in between midnight and dawn. The clerk sending the

last message added "Good Night," to let the coastal offices know that

there would be no more until morning.

In this case, the forecaster ended his advisory with a notice putting

all Gulf offices on the alert and the clerk added "Good Night." And so

the offices received a message ending with these words: "All observers

will remain on the alert during the night. In case the barometer begins

to fall and the wind rises, Good Night." This created a furor in coastal

cities on the West Gulf and it was several weeks before the criticism

subsided. By Sunday morning, however, the gusty wind had not risen much

and there was no great fall in the barometer, so the weathermen had no

answer at daybreak. Soon afterward, however, the weather deteriorated

rapidly at Corpus Christi, and hurricane warnings went up as big Gulf

waves pounded over the outlying islands into Corpus Christi Bay and the

wind began screaming in the palms.

Around noon the worst of it struck the city. The tide mounted higher

than in any previous storm of record, except in the terrible Galveston

hurricane of 1900. Much of Corpus Christi was on a high bluff above the

main business section, but the latter and the shore section to the north

were low. It was after church and time to sit down to Sunday dinner when

the final rise of the water began to overwhelm everything. The police,

sent out by the Weather Bureau, were knocking on people's doors and

telling them to get out and run for high ground. But these low sections

had survived a big, fast-moving hurricane three years before, without

nearly so high a tide, and most people thanked the police but determined

to stay and eat. This decision was fatal in the North Beach section. The

road was cut off and nearly two hundred were drowned.

Down on Chaparral Street lived a man named Clyde Simpson, with his wife

and seven-year-old son Robert. The boy's uncle and grandmother were

there also. They were about to sit down to a big platter of chicken, and

the boy had his eye on a pile of freshly fried doughnuts. They had been

out standing with other nervous people to look at the great waves

roaring across the beach, but after a little the storm waters had forced

them back and covered the streets. Now the water was rising fast.

Several houses had come up off their foundations. A large frame

residence on the opposite side of the street floated across, and, while

they held their breath, missed them by a few feet, struck the house next

door, and both collapsed. The elder Simpson said it was time to get out,

dinner or no dinner.

The family went through the back yard, the nearest route to higher

ground. The boy's mother put the dinner in a large paper sack and held

it above her head as she struggled through the water. The father carried

the seven-year-old on his back and brought up the rear, swimming a

little as the water continued to rise. The grandmother, an invalid

strapped in a wheel-chair, was pushed and floated ahead by the uncle.

The boy worried as his mother got tired and let the paper sack hang

lower and lower. Finally it hit the water and the chicken and doughnuts

sank or floated away. That scene was etched in Robert's memory, along

with the battering of the winds and the tremendous rise of the waters

over the stricken city. The family survived.

Looking out of the windows of the courthouse on the edge of the bluff

above the business section, the boy watched others struggling toward

higher ground. Afterward the family returned to their house, smeared

with oil and tar and by dirty water, floors covered with sand, mud, and

debris. Robert saw death on every hand--dead dogs, birds, cats, rodents,

and one neighbor who failed to get out.

In 1933, when one of the hurricanes of that year crossed the Gulf and

threatened the lower Texas Coast, much like the big one in 1919, a young

fellow drove all the way from Dallas to have a look at it. He was Robert

Simpson. He never got it out of his mind. Finally, he joined the Weather

Bureau, worked at hurricane forecasting offices and in 1945 "thumbed"

his first ride into a hurricane. After that his enthusiasm and

persistence annoyed some of the older weathermen and bothered members of

the air crews who flew the big storms both in the Atlantic and Pacific.

Simpson made up his mind that he would use every opportunity to find out

how the big storms were organized and what they were geared to in their

movements, regular and irregular--the gears and guts of the THING. When

Milt Sosin lurched into the center of the big storm in 1947 in a B-17

and looked up to see a B-29 high in the eye of the same hurricane,

Simpson was up there with the men from Bermuda, trying to find out what

steered the monster. And on this flight, with a B-29, they expected to

come out on top at twenty-eight to thirty thousand feet, according to

the theorists and the textbooks, but they broke out just below forty

thousand, still one hundred miles from the center. From there the high

cloud sheet should have sloped downward to the center, if they were to

believe the accepted doctrine of circulation in the top of the

hurricane. But they were shocked and chagrined to find that the high

cloud sheet--the cirrostratus--sloped sharply upward in front of them,

rising far above the extreme upper operational ceiling of the B-29.

And so the superfortress turned toward the center and rocketed into the

high cloud deck with misgivings on the part of Pilot Eastburn and

Simpson. The latter reported:

The Hurricane Hunters · 第 18 / 20 段