New-York daily tribune. [volume] (New-York [N.Y.]) 1842-1866, 1853-08-02
,rd nn. hpndrd mss rom ths co.st ne resuItants

ard ore hundred miles from the coast The resusnts are
from TIE lsnd and At nchery points 10 vin'er out me
great from the sea that the annual
sulisrf j. from 30 deg with constant force OF
u in the estimated notation OF force The author II
referred snalogss Of these continental .nonSes
~ noy-m pis with thos 81 the E<st-rn Con
tinsn sucirg hs observations Of Prot Dove OF B-r
I'm A. given IN tn EdiHba "a Nes Phtio'0psic1 J0H-ai
regsrorg The indian monsaons the eAsI WINGS OF n7 nt
eru Coss Ass ard the north WINGS from the Polar ga
He shows hv COMPARISON Of bar meuc means or h- on-r
en portion Of the year the inducing cs1se OF ins genera
cot;ir.ris rarefscnon 10 Atmospheric circus
tot les really a. TIE base Of al The amOspaer, condn ms
observe in ADV single portion 81 the eNto Dove
sud,s the snti, change in his views OF the rsaon
Of these Conditions 10 Europe which have been enforced
by coupgi.on OF observations IN )ther paris OF sne Scr
sn0 specially in Asa Our condn ms oOth constAnI
and disturbed dynamic are prominently 7t-rSni- u
and general causes and - ssste oi AOsPue''O
H. ~Northerr OF Texas and the Gulf cos,, no,
coming in the class Of winds Of continental A'pirs
lion hss net been referred IN the foregoing The sta
ti.tcs Of this phenomenon It should De confessed
scarcely cient solve tie sus rons connected WITH
it or even show .irly in sny e1hohs II bat some IN
t.restre facts have been collected snG some <nSos-s
sen. so clesr that il may be proper 20 present them 20
.,ry.op Of tie Ncrhers both borders of their exf-n
sion north sno south has been very well nsce-in.ir ins
vet even ce srer idrn nty with tn Gan u CON
cerpeo TIE PEDRO River Of Western Texas sna "a"
n ouutsps boroeuUg the PecoS i to- line OF distinct
bouIcary not only this pbeno nenon but OF the gea-
climatic coudit IL Of that part OF Texas Inc irregular
arc violent OF New AeNco are not analogous 10 'o-
Norher htus after from the Nsrh Their Characters
tic. are n oecid regusrty sndtn- most
,boropgby local on the noriu Fort AtknsOa =; the
rg Of N, Aksrsss is also eyond them sui indeed they
e, n limited nearly 20 the district OF the soun e,s' mon
or though reaching in Smodh-d character '.rnrr east
aid farther west At the south, their limit Is r'mH tn-
waters of the Gaf-pr-vsling, A. have been assured
sontunes within sisht Of the norbt"Srd WINE tue ~
pring trsde ~ind IRON the east conlusu Us 0'
IN. following summary presents he positions that seems
% b. established by osts which have been oonred IN
sxn UhelOneu.
b. 1-lss Plains.
The southern Monsoon is claimed to be 4 true D,.yf
NOns00H sno analogous 10 the MONSOON ALe Desest Wins
ITO Norh,r, are considered a. pecGi.r the physcs
structure 81 the continent ard IT, relative position 10 me
Gut o. Mexico, but not Is having any Necessary r-suon
10 th4 south wno 10 other districts than ihose II
Tn mir o.cnpusctiou Of both these phenomena from
IT, ch,us,s occurring on the Plans Mountains North
src arc r. III the climate Of the continent else where gen
-r.y i particularly Insisted upon p~curAry zeal ana
lut,c q arattor traced 20 The position OF the Districts
in which they brtsren the lines OF NAKED eaec,
TIE systeu 81 general pher; CIR ua1on snd IN l'tl'
tud.. which At SEA vould oe belt OF calm.
As true DrsaIt md ot aspir." a. th- sou h-rn winl
II t-xs i uou yltADg wisd -asin< Ia enp-f
xuT rsTtaciuu aLd e1hsu-ns Hs~Ii va rAniess us
II e. D., oDd bcb II Goes extend
The Nnrihrr safd-i reverse WIND 81 aspiration
he positive laws which cannot A. present oe n t-
bu ,ue negative positions ar taken a. oAoss Il J. Mt
WIG OF PROPULSION from he EcSy houut"us or TON
n. psits Il B. pot % the primo pa, oody OF
- AIM, sphere within The hnt ot cloud i"rm Auon i Is
not lreCyag WIND from rs Al VsaIe' oH' "n7n Al
tended ~ IF sly amount hNs nearly reverse cur
fut ID, - u rom winch the principal precipitation taxes
pa,, ordinarily anAsg u o fne rtn rast ana ,olh'
-, arcs at. lcs aeG.rsl th- United states.
uhi,b procr,,. tscs ssr contrary % their general
,u,ct, D. .uc sWass secondary an" IA th7 nature ct
c, u, queues q great general d h"t
.pparef On, really - from the iIct OF
III LIstl ct the pbsuoDehon TAXING place n NJ o"
H. ss.unso cause Il the phenoa,.ns Of the Norther
H. e,aoTouary because excessively violent 10
. m-ifs D, suG d-n as,-t of r,re1-d .nt sau
ra,sc youns TIE aeern UA 81 The Coll >nd on
III cssis occurring Iu-guisy from ~ pc uliar coaior
a.. 81 The @tc COS ILeu There, eho ihvr position r.
l,ii,e ro tie Trace Viud-.
Thet4u,t.iisaiions have been mainly reported under
the sanction - he sutrouan lnsGtion Hded oy 'h7
I.Isols tEoIts 1T hr BoOg-t Lieut. ''ecb, OF the :
ANN, has recently Undertaken explorations IN the Yves
H. A. tto.. ufIoi these inquire, Nnd IN the course %
10. .uF-yilgs denta!y sard 40 "a an extended -
~ Il obf stni mair by French physician Dr B.r
M did, n tie Oh ri tsof rthvro Nix c' sb"u San L-us
F,,.i sIo ne inter,r but m,Iny ia MA'smoros
H. E-anoius instruments we're iurnl'hro hin by S'c'e
y Piyfciais at GeneYa anc d. reported avs oo'-fN>
lions h-e Ai.rVard continuing long rsr7- for ms pr
yAie .ufposts On bis cesth ear or So since they tel
ufo haucs OF Lieut. Couch and Ar preserved la the
Smithsonian Institution 10 manuscript
The Z.IiocI ItglL ,e f,,,l,.al opo>acoer,o f Hrors
ana N, J0stt.a = me Iltsf IN spac . rhh M vift,H
oj Inc soo, sy,t,a,t etd, SEC b. DANitL N,UcH.N
~ CluCinu4u
Dug tL4 ist year endeavored to trace the origin Of
H. Z,o.4,s Ia ht the effect ~hieh Voting m-dium
to- ce, s,sl spsce- with the motion OF transit.
7
Locits bch visit our globe a. shooting stars.
The rr,.tria origin Of these bodies well the
NOV, Of system through space, - generally adj
uit.0 and even he ex-tsnce of rare medium 10
uough 20 eiies rega rded hypothe,c. is t'rdugt
Hon bodt proved by the exact sccordACce 81 numsc
"r-iy,s On ny recent eshgaton- on this subject
have taken ino the Effects OF planetary At
fainu Cd such booze, small, light enough - be
c. rfrCtd b. The and this cause which ~ hr-
neglected nooe- he h-ory considerably and enables Il
t. svtrs iacts tor which It could previously give no
e'I.n.Sn o., ,s, with rs.o4ct 70 the medium both
tayiug the Sam motion IA supDOs1on which uone sill al
nit De orbit 81 BIS attendant should continually diminish
HuboLt undergoing much attraction IN form But " ne
u.y-t Iap,oy tbr Ugh thi. rare faid he small oolis
Which ate Id him Will ,usian greater dinlnut'n If We
CITY iron- iis one side Of toe os Of his ma
ion than they sustain IN describing the opposite po,u IN OF
tnr croft continual increase OF eceBtTl ~ al DE- the
r-e,s-.ry Il this unequal resistance out the
ucrta.e x be- arrested as the dies approach n-sr the
.uu on 81 the greater density OF the medium IN
Ia. vicinity Il evident, however that the great vara
Oh il ceisty which would expect 70 ind IN the part
Al the tuid which atmosphere for the SUI, must
m great measure, disappear AZ considerable distance
fr, bin IN qencs Of his great velocity and houSh
liz ATTRACTION prevsLts the relative motion # The m7dum
ff, u beng r@culBear the detection Is reSy
eyeTy ride all not therefore prevent the sougsnon
o. n, ueteorc orbit. Were medium al rest would
h. Isiursio e1psct that the peb-,o OF ali these
should Dc sfusi,d between the and the POINT - which
he j. moving His opinion have confirmed o. mttHe-
/ Y stc2l invest. CATION which shew that tue
tion If Their usrtverse principally depend
/ on tbs -- Of tAic- the angular dislsoc. between.
if.ir perhelA ana tn point IN question The small sac
ar T. Al variety the bodies will this eIu2On 20
Dr. ucersts those sriI from planetary action aud
ali thus prevent any Considerable deviation Of the
we're axes iheT roIs from the ne Of solar motion,
whenever tie lat line has small inclnstOa 70 their
psi.s Indeed their planes hpE-v-r they might be sta
seG shc I'D gradually FprOach his ne aud ta.y c"n-
/ ,o. I'D il Tie movement II the nodes by which this
oaI e Is produced, cspends the angle the ns for
th each plane Ia the Of the light bodies under con