The Anderson daily intelligencer. [volume] (Anderson, S.C.) 1914-1915, 1914-02-06
nf If RlfE v1cny aid.
9sGGVA -. AAeallA Aiverllzln

Dc subject 20 error Because the steam
snip IIii6iiat &c. delayed 10y fok or Inc
cars In5Bht hlees with an accident.
Storms, like pineBpples. as a rnte
do not originate IN. the United States,
They come to us from the Philippines,
Japan, Siberia, Alaska, Canada or the
Gulf of Mexico. The watch r burean
gets cable, telegrapliic or wireless
notice OF the foreign storm. station
after station. Oh, vessel after vesseL..
reports the ssoEnss arrival in It's
neighborho0d. so that the general
direction and rate OF progress can be
detefTalnee very nearly. In fact. the
. arrival OF some storms ca1i be fore
told ten days IN advance.
fI1le foreeasters watch for the
reign OF low harefieter, which is the.
storm centre around which the sinds
blow. This 'whirf or eddy moves bodiS
~ forward with the general eastward
drift OF about ESQ miles a tlay I'm our
latitades. AS the lines Of equal pres-
sure fiaoDars) arpnnd the low centre
crowd closer together, the winds
attending the storm Increase IN force.
The foreeaster determines the direct.
ion of movement OF the storm
and its velocity.
When weather disturbances are re-
ported the fOrecastefg know from ex.
perience how long 1t takes them
to reach our Paeific, coast, and then
how long after they Tlif reach the
Atlantis coast. For example. ifa storm
coming fronf Siberia dirfts eastward
around the north pole ana reaprsars
In Alaska; It should appear I'M Wash-.
instoA and Oregon tf abuur two d{ys.
should get to the Great Lakes In siy
days and to the Atlantic coast tn
seven or eight days. 2
unekepeeted conditions may delav
storms or divert 8ienr from flis
Etfhig!tt track, jiss ifs d refrigerator.
car Haag be tiirSWff Off ttsyseApfiitif ~.
be SHIPPED by ncSfdeht on a Trapa
road. Some OF these storms dariese
themselves by running into regions nf
high barometer which are CT greatar
magnitude and extent than the storm
ITSELF Some OF them, however. travel
completely ahaIAd flfe vsoyfd.
svks5T5 t15 .t5s15 Jsif iii tie cpiti waves that
come thtO the United States from Cl4iz.
ada and Alaska the weather tttrentf
Studies the CallaGiaa 81 weather reuoFts.,
England sensis reports from IceihnI
the British zsles and contine1Itsfi
Europe and daily reports corneI from.
st Petersbute On the eonfiitsons In.
Russian asi Siberia ~ as.ts's
Tae RaIne btstsesaltie system ftshd
In tracing fhet track fla, storRiiis nm
IA !, III II N M, 7
frosts!t 'f,Stss ~ i ~ y.
! Tloed forecasts All mai g!aaitttiieh !aait in
the same wa al II faliati6f ss Jt0s 4iih
amount Sf rainfall al The head Y aters
of streams flfs cause fioods he eov-1
ered dy teseaFab phi e fey0fts stsfItI IL
local fEefa us ain reaches
the main sellnunei Of lie 4 of siIe
lssafsss Ia flslki "a :,
stieeessiye g;sl esflg stations. rec, rists.
ards lss.s e i.ss!s.l.
sssgs sitt Dss5sii fitiIt. an IT ser station
so miles down the aiisstssfpbi. tTiiIs,t
plan isi FOL lIesSed ali the WHY down
the river, and at eaeA point faiIi NJ
loEansc lsai MADE for tie effects of I
water FROM tributaries and from ad-
di.ie..s.sssss .s:.! s: I.ss..f "a -
snlt the recent 6bseryations In
thu n; flood the people OF. CAIRO,
Il 80 rr.Ilg d lyeel: or Ten days In t,S- I
rane. The Pittsburgh district can be
given only ~ TO "a hours. notice, be-
cause a food is upon, them within
: hours after heavy rain storm.
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