The Vinita weekly chieftain. [volume] (Vinita, Indian Territory [Okla.]) 1902-1905, 1904-06-23
CAUSES OF STORMS.
WIND MOVEMENTS THE RESULT
OF VARYING AIR PRESSURE.
Natures Expander and Condenser Of
Air on the American contin-
ent--course Of the
5torns.

Few persons who grumble about the
weather know, or. II knowing, stop TO
think that the storms which sweep over
the country periodically are only the
result OF the processes which Nature
has adopted TO ''yentilate' the atmos-
phere OF the earth and make the globe
habttable Storms are simply wind
movements, and without them the at
mosphere surrounding the earth would
become foul and stagnant, says the
Cleveland Leader.
Wind movements are the result OF
varying air pressure. as measured by
the barometer, High pressure Is pro-
duced by the condensation of dry. cold
air, and is followed by the precipitation
OF atmospheric currents from high al
titudes toward the earth. Low pressure
comes from the heating of the lower
air strata. and the absorption Of moist
ure, and is followed by rising currents
of air.
On the American continent there IL
an air expander as well as an air con-
denser The expander Is located over
the equator. while the condenser is
found in the high plateaus OF the sas-
katehewan country. north OF the Da-
kotas and Montana Air heated over
the equator and 6lled with moisture
there rises and rolls northward toward
the pole, Near the thirtieth degree
north latitude II drops toward the earth
and encountaes the masses Of dense,
dry air, which are continually being
piled up about the polar region.
IL is the continuing conflict between
the low pressure and the high pressure
which produces the storms Each storm
has center. and that Is the point at
which the atmospheric pressure is low
est The storm center is called the
low and II is the progress OF the low"
across the country which produces
winds that accompany storms These
winds always blow toward the Glow"
and are high or mild as the "low"
varies in intensity.
Many of the storms which sweep
across the United States originate In
the caribbean sea or the gulf of Mex
leo. but a large proportion OF them
start In Montana or across the Cana
dian border Storms of equatorial or
igin. II they strike the land. follow the
Mississippi and Ohio valleys. as a rule.
and go out to sea over the gulf ot 81.
Lawrence Sometimes they 60 up tho
Atlantic coast In the form Of hurri-
canes. causing north or northwest
winds over the greatest part OF the
United States east Of the Mississippi
The storms which originate on ths
plateaus OF the Rocky mountains are
milder than those that come from the
gulf Of Mexico Sometimes they swing
around over the middle states. but
more frequently cut across Canada
north Of the lakes. and II they take
that course In winter they are followed
BY warm weather in the northern
states.
These storms Of low area cross the
United States periodically They aver
age eight month from May 10 August:
zine a month from September 10 No
vember and In April. II a month In
February. MarcL and December; and |
l2 a month In January The average
Gelocity OF these storms-that Is their
Onward moyement-Yarles Il Is IS
miles an hour between June and Septem-
Der: 2e In October: 30 in November; s.
o December; IS IN January aud Febru-
Try: 30 In March. and 20 in April.