Fort Worth gazette. [volume] (Fort Worth, Tex.) 1891-1898, 1894-12-23

ST. Joseph, Mo, Dc. .s.--Ay last
bulletin gave forecasts OF the storm
wave to caoss She continent from 2ist
to 2esh, and the next will reach the
PaclAo coast about thu sdth. en-, tae
Western mountain country by clsse o,
he g7th the great eeutu.l valleys from
sSah to Goth and the Eastern states
about the Sist
1yils disturbance WI probably pass
along OF south OF the 10th parall} and
will be followed by ssyers cod wuve.
Warm wave viii crOss she Western
mountain country about Inc s6ih, the
great central valleys about the ash and
the Eastern states ab4u, the sOth, Co,l
wave Will cross The Western in0untain
country about The 2ath, the great cen-
trail valleys, woil to southwark. about
the 5ist and the Eastern s'stea about
January =
\ general forecast u J nu ~ wealth "
for all parts OF the uniied S.aiea VIII
be given an my next bulletin,
Cloud Formations.
Analogous 80 thc ideas heretofore ad-
vanc a as to word building "a the for
nation of clouds. ialcctrie on,feuts,
AiNiN WHY lHHtNAA W NaAAAlttHd
pour into the transient low barometer
carrying with them hhclr loads OF meis-
turp that have been gathered In the
far-on seas
There must first be an organic center,
an Clecirusph re- win Its glnal clcn-
tric and Induced magnetic currents,
its equator cNtcgdlng h grig nttly, one
of iH p1lqa piating upwlFd, tho other
downward and the whole rotating "a
ats axis,
Into such an organic hidy transpar-
ent moisture is carrl. by Jlcctrlo cue
rents and deposited. thereby formlng
tine clouds.
Every part Of the storm center IS as
tie whole a. every atom composing
the earth has an electric ND mavnc Nv
org niaation. an dccirospl ~, ons T.
tuted precisely on the Aamc llnn az
that OF the w0ole carth.
Clouds float IN aectons sometimes
large, sometimes quite smaql and thc1o
seotiann are held In form by their elec-
trosphorea
That which Ia generally called a
weather disturbance Is composed OF n
pair o. bnsomcturs, a high afld "a low,
which are electrically come ted
throueh their poles and through their
equatorg.
in the low barometer the currents
along the horizon converge, move in
ward, toward the center Of the low
along It's equator, The currents move
out Of the low, upward and down
ward BY way OF ita poles and connect
with the poles OF hs mate, the high
barometer,
The current movements OF the high
are exactly the reverse OF those In
the low, the two constituting m oloc-
trio pair, From the earth below ard
from The atmosphere above these our
rents move along the poles Of Che high
barometer toward IT'S center and then
outward through Its equator toward
the low barometer
Thcse great centers Of electrical nc
tons. one called "A low and Tho other
n high barometer. constitute the force
Of cloud formation. They are eioe-
trlcal and conform to all the laws Of
electricity, they arc magnetic and each
constitutes n complete pair OF mag
nets and IN their relations 10 each
other constitute pair Of complex mag
nets. They also each constitute an rlco-
trosphcre. the high being OF that kind
which dissolves, disIutegratcs mattori
destroys worlds and carries away the
debris TO build It into other worlds
and the low being Of that kind IN
which worlds are formed and matter
condensed.
II IL inc permanent naNn UNINNl'A 'NA
~ the Atlantic. the Pacific and the In
dian oceans that evaporate the wat
ers and carry them 10 the semi-annunl
loag barOmetors that periodically over
hang the contents. Each OF the three
oceans are divided into two parts. north
and south, and over each Of these PARTS
is permanently located Il high bsrom-
eter each covering the whole VI ita
division OF the ocean.
4. 4 IL IlrHNa md
the moisture that forms the clouds and
rain for all the countries 81 krrth
America lying east OF the Rocky noun
tainB aud from the north Pacific nigh
comes the moisture FOR all west Of the
RoclsieH.
Storm ccnfesr are very seldom or cx-
tenaive as the low IN which they are
formed We see the clouds fDtm in
summer making a complete storm oen-
Ter although only few miles. even
not more than one mile In diameter
and there may be at the aai1e time
hundreds OF other small aic'm cen-
tiers In tho Same low which N always
from 900 70 1000 miles IN d'imeier
The tornado IL another instance 81
storm centers and there may be
dozen tornad0es al the raine lime ~
various parts OF the country but All
IN the same low.
formations are not seen IN the tran
sient hilsh barometes. The general
cloudy weather and genoinl rain or
snow often occurs between tle high
and low barmetcrs. In fact there "a
w2iere the most snow and rain fail
occurs and this is called In these bull
letins The storm wave.
The transient low barometer IN which
the clouds are formed pasB entirely
around rhc earth aud consequently
through both the permanent high aud
permanent low and deoreaHlng while
IN the permanent high.
Starting from the coast Of California
transient low passes eastward
through the periodical low which COW
ers the westefn half n rhe continent
where but lilsle rain falls because
while IN the Heni-annuai low che tran
Rien, low win absorb moisture and not
preeipiiate It.
This eastward hound low passing
into the Atlantic on the Carolina cnest
enters the permanent high Immediate
~ after crossing the MisHireglnR nnd
the water r. squeezed out Of Il caus-
ing heavy rains.
Marvellous Results.
Prom letter written BY Rev. J. Cum