New-York daily tribune. [volume] (New-York [N.Y.]) 1842-1866, 1853-08-02


,h cay ssioIs new fibs.9 5eoie
fI.tt > , 49,, IS Fourb 5,v before .........e.s
ThiId day teiore...--''. ilra qy ooie
F,.f esv before .....6.4 First day before
Th.s. numbers Indicate bur Slight lewiston from o.. y
Which tie average Coudntss 81 the whole p-rod no
rur.sriipg sky perfectly ry-rca,t In other wards,
e,aiy two ttrcs the Ky a. GrcenaIcA l.. upon An ave-
rsge covered With couos TIE greatest departure from
n mean occurs the 5.cond 0.y ser iu eh-n tl-
.yrrgge o. J. This might be -usp ecied % indicate alas
II MUIR but such Inclusion i di-coun'"ntuced ~
~. ict that the am ut 81 cl'uiL'ss on h- "'~r"u
YEAR very unequal H. l-f tn aver " r"Lia~ss
or he - cCrd ca, alter uli VS. only wi'h D, D. ~
v Nh. .v.rsge result Of th- ssr- y-Hr- In l-i! the
av.rs2. for tie second day aii' full 49, B. " D.
cx tie eentrl mean Th- av-rsge o. the rrmN1ng i've
-rr- 3 hitch is Only bel"~ the general me- An for
the entire period
amer fbat The middle Of the int rva, h' correspond
"a new oon first qusrter full moon aud last quarter,
hall Obtain he sVeTsge cloudbe,- At n-F moon o. D.
frsi quarter = full moon r. = ana last quarter o. re
mi. ufich may be- pronounced entirely Identical and seem
10 o.mopsii~ie hat Sir John Hersohes meteorological
pct j. III il gi-o Dt'0n'htNe
tn. i. calculated % conceal the fact claimed
b, Sir John Herchel inAsnuch As have employed me
s1esge ciouduess OF each entire d., whereas the full
non i only claimed 10 exert al influence when She IS
above tie korzn do not scmit the orcs oi ts7 Oh
tol for # The iu moon when ABOVE th- horZoo e1eris
Al Ia 6sipat. the clouds, such an inf~nc- Ought
10 sIIexr In the rage udness OF the twenty tour
hour Thi. conclusion only b. avoided by -upPosng
tt the tu noon when below The horizon. e1srts posi-
iuturnc. on thu coud, contrary 70 ~ht pfnllctd
vi en h. is above the ron ana tbs one ought
"a be ust A. pspable the other and ough not 20 have
.c.reo the Of shresd IN observer SIR john
! Herschel
IN poirt lave compared th- observation, made AZ Mi
pelt Oh ib- GAYS moon. hr,i quarter fu moon, asd
! lat Quarter for tie enirs period OF seven years.
According these observations The average cloudiness
A. nicusht on the day Of new moon is A. the nr-t
Quarter at full moon, GO ana AZ the lat quarter J.
he Fret three numbers may BE- pronounced identical WIN
J 80 entire p-D0i AireAly
/ -sflaIed The last ight be suspected - indicating
.ei.rsl law but compare The moahs for each year
:. tarsi.y We ha find that thy range rm v to %
.h.x that CAUSES which independent OF the moon
,ee exert Dc erfu influence upon the degree Of clou1
n..s Moreover see that IN la And ls' the skY vas
remarkably clear at TIE sst quarter "he ihr .V1rAS- 81
tb Aiile Year almost identical With The results
! ~ he 9th, yeriocs Of the moon
romri.op therefore !, ads us 70 the result
n. former viz that the Green ich observation, which
i,h the q, cree coud ot the sky eyerytsO hours
i. b No oay for years give no cOUnt-nznce 10 th-
tat c.iu 20 bv john H-r.chel and We have .n)ler
,Ismpe Il The danger OF dra~Dg general conclusions ron
ot,.rvsti IL Oos. " Treasured up IN memoTy without test
| ug item by reference % recorded tAoie;.
NJ gy-Bot Sons ara Nytser' b. LoRS BtoDcEr,
w.. sr .en,ed by Mr. Lorin Bodset Of wash.
ug,'n on the uhessi Mon-"on, and rrner Of I-1ss
And the Abu, rs Atmo phetc movement Of the 'rih
! American Comment generally hr bl"oge, aiiressed
Al. ,r,r. ser. Of observations r-lNy- 10 the h-tere
s- pb roneua of hat portion OF tie North American
Coz II lying west of ih- Ni-si--ipp Rivera region
which Until recently has been almost anknoSn IN regard TO
lie condition. Of climate Mr bl"dgst referred 10 tue pc
cuar heTc nents bat are sho n e1s there
iuel tie observations Of army officers attached % the
nt-fy poss by the I'D oi officers charge OF sp cil
srV,ys and by individual Observ rs-the accdml .ted
oos,rvAroIs of three years har thus become sg
ent 10 thros great Ugh; on thr more striking pben'm-ra
Of these Pacific ana interior eli mates The author pro
To refer 70 The peCuA Atmospheric MoF-m-nts tlAt
/ AZ how "a exist
TIE whole Atlantic and Southern Gulf Coast presents
u. With more r less marked Alterations Of land aud
! ill eHrr NEW ~..Ha
IL Which and ihr-r solution, We quite "A niii4r.
Bat toward the westsrn extremity VI the Cult Coat in
Texs- tbs becomes msgnia-d quite O-yood the ordinary
JL-Iomtna - laic Anc sea or@r-e ana develops True
roIsoou or ind Gay aud ught or months
g.tl,r AZ ~ mouth OF tts RiC Graud-. and bet
ih 2. III ara Corpus arr the max mum effect p-O
terror Dssesi Plaza called the Par7 E'tqclf0 o. StaEsi
Han sId t"s. The whole district bounded ny the
b. Grade tie 81 Pecro and Pecos oa toe sout F-s
&c u,r-n- gradually IN - low psin Of I-1is oa me
49, tom Nay 9, November n IlsSh4 lover attitudes
On ih- N,st,ru coast q NJ xco the trade Siac o.. TIE
rc. QUITE U.uralZ-4 - cS-s-s Analogous 20 tbo-e
81 n, fr-t uh-roa-fa. Aac this tr soce distance a. sea
Fcr scr pofn 81 TIE suu Drr months % July r-viy-s
he ;Isoesi-t. ard tloss >outn~ - vud 10 The direct
t-ih o.. IL siheas. trades L-l- AAlry fully suosAn
fsi.. tbs reversal o the tr.de Vn4. 81 certain INES
,t .gus 20 rhe i-s- ID Velocity nOIgh tla
h.rvsu oftt- M-ii, coast a. Maza n, and 81 b.
fs rs-n quite r. -lA aLc % Ial amount Such only
I'll. tte rrsl ~ II I - e. 81 vessels could MAKE
On H. Cain III, ssf coLinr u vino IS experience ID
Of usrzec chsr. a. q attrac. great attention Tae
r.h ~ roitr thves gnc re Uni4l ng occur
.v-r, Sumner cay a.c on lie nusc AZ scarcely
-s- = az through he screr 20 amount 20 !an4 wArl
aspiration As this ola-s however without being led
b, h. circulation 81 ,U-i.c- suO,phsre usually eceivec
"a tie normal las not ihe absolutely c0Dtlng
,fa-se--r Il would have accorded nearly 4ccOrd4l
With mat circulation The Monsoon ii I-xa. nea-
~ accord xifh this circulation expressed th-rs by TIE
orineast trade eri-rs ths Gulf objected by local cir
cuustsuCes exaggerated breeze az the GUl
,oasfs-ilN more readily blends sih that movement
and d.d. cs merely 70 true southeast continuous wac
Z rtirr /. partly trade ana partly Monsoon
Nj l. % get nifOducs nrtiees o ths resultant s-mos
pber,c movements u the Lower Valley Of the la Gsands