Fort Worth gazette. [volume] (Fort Worth, Tex.) 1891-1898, 1895-01-20
as WEATHER FORECASTS
= WINTER STORM COMING
NEXT WEEK.
,.x lie a Drouth I'm April
~ nut 1t VIII BE In the
/. c,,matoIogy-How the Earth
(,,.. and Exhaustn Something

hid the next "'i
ast about the cath, cross the
4, mountain country by close of
4 u great central valleys from 26th
4 and the eastern states about
H..
will be an ugly winter storm
I'M be followed by a severe cold
In blizzard.
kyarm wave will cross the west
! ,untain country about the 2ith.
3at central valleys the 2eth and
states the 2Sth. The cold wave
3oss the western mountain coun-
iout the 9th, the great central
4 the Goth and the eastern states
Ia.
5atIons are favorable TO an ex-
1 drouth in April and May, prob
A greatest extent In the northern
II / will give q full long range
X of this in my first February
This will be of great lmpor-
M farmers and before giving a
Ia forecast the calculations will
tefully complied.
3puth at that time would not very
I'm damage the northern states.
4 some sections Of the south e
4 be ruinous.
\ Lour cardinal Points.
Ia study of Climatcl0gy from the
boint OF the new system of me-
Bcy laid down in these weather
hns, there are four cardinal points
a northern hemisphere to which
..iox meteorologists give no atten-
y four cardinal points constitute
4principal respiratory organs
IN which the earth inhales and
\ a somewhat? that is probably
&ctricity or magnetism or either
&ry closely related to all of these.
ID these organs are inhalers and
nhalers.
'the northwest coast OF Alaska
Where the Aleutlan Islands branch
BIN the mainland Is situated a
tual low barometer, a perpetual
Temperature, where the atmos-
His carried upward in u spiral by
currents of that some
"A which the earth exhales.
II annual temperature average of
roint is is degrees warmer than
Serage OF that parallel-G0 de-
Eof north latltude-and that OK
u temperature affects the climate
ID the Pacific slope of North
sea, causing 1t to average warmer
ID otherwise would.
N perpetual low is about 5000 miles
bmeter and has Il spiral whirl
" to that of Il tornado, hurricane
Ejnmon cyclonic storm. Around
inter Of this the winds move in a
Il 50 that on the east side of its
y the winds blow from south to
4 thus bringing tropical warmth
A Pacific slope.
ern Asia lies in the west side of
Pw, and the winds coming from
birth bring an arctic cold with
= and this causes the climate of
b Asia to average many degrees
than the same latitude in
a watch with face up and the
Xof the winds and waters in this
Hual low is contrary to the move
of the hands, and the gulf stream
papan flows into and through the
side of this low.
II the opposite side of the earth
<fhe Behring sea is another and
.fimilar respiratory organ of the
d the center of which is northeast
Wand, and there the annual aver
temperature is Al degrees warmer
e he average of the same latitude
~ the earth.
Fnland Is situated in the western
~ this perpetual low and for rea.
8xplained as to eastern Asia is
y degrees colder than northwestern
"a, The West India gulf stream
&lnto and through the south side
= perpetual low.
v well known that the climate OF
Pand Is changing to colder, and II
Felandic perpetual low is found
explanation. BY observations o
fagnetie needle in Europe it /,
mat the needle variation slowly
III indicating that the Icelandit
4hile 1t is called perpetual, is really
a changing its location.
oSo the magnetic needle at Lon
%pointed IL Ia degrees east o
4 IN 1867 due north and in 1871
a uegrees west of north. Thl
X Is not due to the change in tn,
geographical pole of the earth
change of its magnetic pole
ara. Our scientists who discus
yphyslos or terrestrial magnetism
H. recognize the Icelandic AM
III sea lows as magnetic poles
&hey are such, the difference be
Hiat they are the opposite poles a
ifed with the magnetic poles II
#teflors of Asia and North Amer
-erVauons In North America sine
#now that the magnetic eastern
ZION of the needle is decreasing
|ne western variation increasing
would indicate that the magneti
pole on this continent Is movin
8srd, and this is in harmon
we westward movement of tn
ulc magnetic pole.
lagnetism the Icelandic and BeI
NV lows would be called sout
eue poles, because In them tn
spiral movements are agains
uh or opposite the watch han
ihents, while those magnetic Ger
4 y the Interior of Asia and Mort
iea are properly called mort
etic poles because in them th
z movements are downward an
Itments.
~ are four magnetic north pole
~ Northern Hemisphere. two {
4 developing what are called To-
Eielers, one over Boring Sea an
,ner covering ocean and countr
iceland. The other two develo
q are called high barometers,, OF
"g the north part of centr'
4 america and the other GOVERN
4eastern Asia,
q me west side of the baromet,
n magnetic poles the climates al
Z ana on the east side very col
4 the reverse is true of II
4 barometer north magnetic poles.
u ~ the above 1t will be seen thi
4 sated 100 wears ago a movemei
seru OF these magnetic centei
4 cause the climates to grow wa
Nv northeastern Europe and mort
#rp North America and colder
#liRnd and norfhaaqtar Aata