The New York herald., 1871-10-21


begin feel me proximity OF w..sr they resum. their orig
nal force and often surpass It,
II Besides force. attracting the areas Of low pressure
na,e s.o 70 consider the pressure Of any area OF hgn
%.S %Sd 5;.s siIsa:s s sasysisas
"a extensive cycone before IT, so AS TO undergo quite
Thu. We dnd that there i a somewhat crcuIar q
Re,manen S,r nga barometer in the NORTH Atlantic
sS nsrA d and
ares OF high bsromser observation shows tia, the storm:
ssm S. s n s s % the o
from let to right e With the hands Of clock toward
80. rnr DrTssSis1Slos OF THE STORM PATH.
a.z sss dy ss
OF which arise from the Of Of high and low
ss $ e ss % os %
others may tides air. &C., &c. arc
E sly g5Gs 5s ". acs an
rsSsny published y me London Mssecog
sSff
a1a ns :ss ma: A
On rs e.: On
which steamers bound from New YORK
:. ss.sxs;d %o'as prs::"r:@s ssss ss
o ssSs: %
.ons each wn y: own cyconc wind em moving
down current Of liver The The
on The bs BE-
given storm centre n fact whshs, clear
Or y S sn to
move ,dr noawaos % h more Rapidly thar ns
.psoysy sSs IL the latitude o. Th.
S:a1S IL .s%espssrs ssss'
the upper currents OF sri the outhwest
Storms extent; instance, tho lev summer .hun
sws ss q :'ns S r.; E or s
Of the and oceanic areas OF high and
%sn'4
ss movement hands Of ~ %ass and % sse Sonssrs
ss Ss
abou; the are. of high IN the interior Of
varying 10 outline and position thus giving to changes
y,
n r. y ss
a II ,1, 70 the yas The
course, with the wind and weather
of sosn: 70 Without
fall at least oscaon Of the quicksilver In the barome
But read by itself and no. connected with other nsru
e snd so natural he Saro
'' now 70 rIsp TaE Low nAnon.rrR.
sanas facing It. he VIII snd he wni Sovas from some point
u
tho Wind eomss WIN face rs$ion q lowest Daro%esr
but tha. from which be low clouds are moving The very
fh,s practically deduced from BsysBslots 'Law
"a "a III S @ o o
as rule TOO o. sr'c.y In nyssgacns upon tho applies.
Insu the Of disturbance and thus it dsdoced
succeedea BY winds the direction Indicated by no law.
and 10 sxywo per cent both tho force and direction were
The force Of local a. any poIn. AMI at any moment
at poin The Vicinity and upon 4. rapidly with
but sac force and direction Of the wind al aay station ara
o very .y Sy the character Of The ground
the would blow with certain velocity win have
Iy Country Ths is due to the lesser friction ou the
and irconsl resistance different ways disurbs
STRENGTH OF TUE wISr
and HI. Sarome,st falling then tho central sTea "a
reaches its lowest; then ull win take place. followed BY
whs ss sas
6s general propor.oned 10 the rapidly the
The intelligent observer however, will carefully consider
"aa % 0s me-; 3. 10 and S ". Ao: a
OTHER nARoMRrBro oosoLUsroNs.
M The storm eee'rs has been spoken O. a. being In from:
% G 10 lis he % w ID. s Il. "
Il as oT from x c sssns " m
that order around the compass. the storm centre passing
by on the north sde OF the ohscrver backs
Tor instance from southwest soueast the centre OF
lowest passing ey Gu the sou side and the dis
fall In the barometer.
Is The sevcrest winds are stated on tho
south and side OF the centre those the east side
IL In lie foregoing The observer has been supposed to bs
stationary should he be 10 motion however this WIN affect
easily into from Of low pressure and
he himself mentally allow Tor tue inuence OF his
ton.
3D. In comparing the readings OF his barometer with
those published the bulletin and map OF this oc, tho
mariner will ind that tho latter have all been eiuced
uniform seaeve and TO uniform temperature Hc there
FORE viii find u convenient 10 bear In the
barometer should he his records and transmit
cm this oce however the original uncorectod observa
tons only desired The following tables show the general
si An allowance for the temperature of the barometer
msdo by noting the Thermometer attached
For temperature Of degrees fahrcnte add 0O3 inches;
for temperature Of 30 add ou0
trac. 0us for temperature OF So subtract ao tepe
OF % aubtract u05 subtract
FOR temperature of 81 subtract cls, for emperatus
OF ~ subtract 0l6 temperature Of lc0 subtract, 0
Those numbers arc applicable 70 barome,es having brass
scales which the most able anerod baromrters
ought not to require any Temperature correction
The attitude above the the
annual temperature but be approximately madc fol-
lows:-
Atfafe of ARitsfe n AID TO