CHAPTER V

THE BAROMETER

Whatever the foregoing chapters may imply as to the whole world going

camping the fact is that the woods are still, unfortunately, for the few.

The woodsman must yield gracefully to the suburbanite,--in numbers.

But the weather is for everybody. To be sure the sunrise that talks so

confidentially to the hunter of the coming day does not exist for the

commuter. But the coming day does, even though the things it means are

essentially different. To the hunter with his seasoned clothes and

well-earned health a rain is only of concern in so much as it affects the

business of the day; personally it is of small moment. But to the commuter

what does the weather mean? Dollars and cents, of course. His business

goes on, but to his person one unexpected shower = the cost of pressing a

suit; one thorough soaking = one doctor's bill. For you cannot expect

the man to throw off a chill who can quiet his conscience on the matter of

daily exercise by watering the geraniums and reading the newspaper.

Weather wisdom is necessary for the hunter; for the commuter it pays.

The hunter had to rely on local weather signs. The commuter can go him one

better by investing $10 (how finance will creep in!) in a little aneroid

barometer. The local weather signs were good for twelve hours at the

longest. The barometer is a faithful instrument that adds another twelve

hours to a man's knowledge. Half a day, or even a day before any local

sign of changing wind or growing cloud appears the barometer is on the

job. It will register in Philadelphia the news of a disturbance

approaching the Mississippi. So sensitive is it that it is the slave to

every wave of the great air ocean.

The barometer gauges for the eye the amount of atmosphere that is piled

above one. If the amount is normal and at sea-level the instrument will

measure 30.00 inches. This air pressure is equivalent to a column of water

30 feet high. As this would make unwieldy prognosticators the scientists

use mercury instead, which requires a column less than three feet long.

And for general purposes this is supplanted by the handy little aneroid

(which means "without fluid"). This is so fixed that the pressure of the

air influences the upper surface of a vacuum chamber, balanced perfectly

between this pressure and a main spring. This action is transmitted to an

index hand moving across the dial marked into fractions of inches after

the manner of the recognized standard, the mercurial barometer.

When the warm moist light air of a cyclone invades a locality the pressure

is partially removed, the vacuum chamber is not pressed so hard and the

dial hand or the mercury subsides. When the cold, dry, heavy air of the

anticyclone lumbers in more pressure is applied and the mercury, or the

dial hand, climbs. So a falling barometer means a storm, a rising one fair

weather.

That is a generality that glitters. If that were all there was to it

weather officials would have a sinecure. But each cyclone varies in size,

intensity, and rate of progress. Some do not advance for days. Therefore

there has grown up a pretty large body of information as each storm has

had to be watched and the barometric movements recorded. The most

important variations follow:

Remembering that 30.00 inches is sea-level normal, if the barometer is

steady at 30.10 or 30.20 the weather will remain fair as long as the

steadiness continues, and on the turn, if the fall proceeds slowly with

the wind from a westerly direction fair to partly cloudy weather with

slowly rising temperature will follow for two days.

If the barometer rises rapidly from 30.10 the fall will be equally rapid

and rain or snow may be expected within a couple of days. Since the

depressions of the atmosphere tend to a certain regularity about the

center of the storm it follows that the reactions will follow the actions

in similar manner,--a long rise portending a long fall and a variable

glass meaning unsettled conditions.

The barometer does not rise with wind from an easterly direction unless a

shift is imminent. In winter the air is so much colder over the land than

over the sea that the air brought in by an easterly wind is soon

condensed. Consequently with winds from the south or southeast, even if

the barometer is 30.20 or 30.10 and falling slowly rain usually arrives

(and rain of course is meant to include snow whenever the mercury is below

the freezing point) within 24 hours. If the fall is rapid there may be

precipitation within 12 hours, and the wind will rapidly increase and the

temperature rise.

If the wind is from the east or northeast and the barometer 30.10 or above

and falling slowly it means rain within 24 hours in winter. In summer if

the wind is light rain may not fall for a day or so. If the fall is rapid

in winter rain with increasing winds will often set in when the barometer

begins its fall and the wind gets to a point a little east of north.

If the barometer is 30.00 or below and falling slowly with northeast to

southeast winds the storm will continue 24 to 48 hours. If the barometer

falls rapidly the wind will be high with rain and the change to rising

barometer with clearing and colder will probably come within 20 to 30

hours.

If the barometer is below 30.00 but rising slowly the clear weather will

last several days.

If the barometer is 29.80 or below and falling rapidly with winds south of

east a severe storm is at hand to be followed within 24 hours by clearing

and colder. Under the same conditions but with northeast winds there will

occur heavy snow followed by a cold wave.

If these promises do not always bear fruit it is because they will have

been interrupted by an unseen shifting of the atmospheric weights. But

the barometer will record them. A rapid rise may be checked in ascent and

the instrument may fluctuate like a stock-ticker. Its tale is of very

unsettled weather conditions and consequently no particular brand of

weather will last for very long at a time.

A sudden rise of the barometer may bring its gale of wind as well as a

sudden fall. But the tendency will be toward clearing and much colder.

A fall of the barometer on a west wind is not common. It means rain. A

rise on a south wind means fair. A low barometer and a cold south wind

mean a change to west with squalls for a while. On the other hand, a high

barometer with warmer weather means a shift of the wind to southerly

quarters and an imminent fall.

If the barometer rises fast and the temperature does, too, look for

another storm. This is often noticed in summer.

There is a slight daily oscillation of the mercury, which, if other things

are steady, registers highest at 10 A. M. and 10 P. M. and lowest at 4 A.

M. and 4 P. M.

If this data confuses bear in mind the simple ordinary progress of the

barometer in the usual storm: First, it will stand steady for a day or so

at any point between 30.10 and 30.50. Then the glass will begin (for most

storms) to fall gradually. As the center nears the fall hastens. After the

lowest point has been reached a slight rise will be followed by another

slight fall and then the final long rise will commence. The rain begins

and ceases at different stages for different storms, depending upon the

wind's velocity and direction.

For every 900 feet of altitude the height of the mercury is about one inch

less. Do not complain that your barometer is inaccurate if you are living

up in the mountains and your readings are not the same as the weather

reports which are reduced to sea level. All the figures given in this

chapter are for sea level and if your house is 1900 feet above you must

move the copper hand of your aneroid 1.95 inches from the pressure hand.

If the pressure hand would read 28.05 the adjustable copper hand would

read 30.00 which is the sea level reading.

One good thing to remember is that a barometer falls lower for high winds

than for heavy rain. A fall of two- or three-tenths of an inch in four

hours brings a gale. In the ordinary gale the wind blows hardest when the

barometer begins its rise from a very low point.

In summer a suddenly falling barometer foretells a thunderstorm, and if

the corresponding rise does not at once take place the unsettled

conditions will continue with probably another thunderstorm. If you see

the thunderstorm first, that is, if the barometer is not affected by the

approaching black cloud you may be sure that the storm will amount to

nothing.

The man in the fields or along the shore has many natural barometers in

animal life. But these natural barometers only corroborate; they do not

foretell, at least very long before. Some are useful at times and among

these the birds are foremost. The observant Zunis have incorporated this

in one of their pretty proverbs, "When chimney swallows circle and call

they speak of rain." As a matter of fact the swallows are circling most of

the time after insects. If they are flying high it is because the bugs are

flying high and that is because there is no danger of rain. As the rain

nears the air gets moister, the bugs and the birds fly lower.

Whether they do this because their instinct is to avoid a wetting or

because the lighter atmosphere of a cyclone makes flying more difficult,

particularly at altitudes, I do not know. For weather purposes it is

enough to watch their comparative levels. Wild geese are excellent signs,

I am told, but it would be a dry country that waits for a sight of them

for its rain.

Bees localize before a storm and will not swarm. Flies crowd upon the

screens of houses when humidity is high, possibly because the appetizing

odors from within are buoyed afar by the heavy air. Cuckoos seek the

higher ground in fair weather and disappear into bottom lands before a

rain. Although they are called rain-crows they are heard in all weathers.

Smoke is as good an evidence of barometric pressure as anything except the

instrument itself. On clear, still days it will mount; on humid days

without wind it will cling to the hill. There is that difference. But it

takes skill and many comparisons to gauge its angles in the wind. It

becomes a test in observation and finally rewards one by becoming an

excellent sign not only of air texture but of the direction of its

currents.

No reference to barometers would be complete without mentioning spiders.

They show a most delicate apprehension of changing conditions. If the day

is to be fine and without wind they will run out long threads and be

rather active. If the rain is nearing they strengthen their webs, shorten

the filaments and sit dully in the center. Fresh webs on the lawn insure

a clear day. But for the commuter, whose time is money, there is little

leisure to consider the spider.

As a natural result of the variation in altitude affecting the barometer

the words which are printed on the face become entirely useless. In some

places it would be impossible for the needle to point higher than "Very

Stormy." Even at sea level a sudden fall to "Fair" would cause a rain,

much to the indignation of the person who thought that he had purchased a

self-registering weather prophet. Disregard the words but watch the needle

and you will never be surprised at what the weather is doing next.

Reading the Weather · 第 5 / 8 章