The New York herald. [volume] (New York [N.Y.]) 1840-1920, 1856-01-19

sackeDiug az il the left hand lie the sweep
hgas appr ach that line very slowly SO ht b'tweeu
Tho fret portions Of the curve are those -here
u ,Ie weI Is nil region q .,, a,assanse'
nicely rounoed lines taund tho worst possible places
stucy the pbenouena the rapidly varying Dars OF the
to tbs overflow Of the Cuff Stream water
coast IDS snd the broad Atlaps he other.
be long tongue that wster from the Guli the cold VA
when saches Cape FIoiia has only tsmpsraturs Of
% TO 20 deg, Y tbs polar current SLOWLY healing up
The intermediate portions be considered ss between
two trstn Que OF warm and the other OF cold water and
as slowly transmitting the hest downward
ward in macs Il auid By c,uductioa. that
az the depths increase in srithmsdcL pro-
prcgressin The curve representing tnis loss ehmsc
and the number expressing the conductOa Of shs huid
know that some doubt .as ihre~n b. ssrtain .xoer
ments upon this law but eauy the beautiful resulta of
Derpretz BY which It WAS proved, cud admit OF no
envelope Of hr liquid These given thu law comes out
rs bas been p9ved since the doubt raised.
Here We have up,n beautiful scale, and with ample
time for eqnilibrium 70 take place, the whole stor
tod Of conduc.ion though mass Of salt water.
logarithmic, and the observations thr Swn into tho
form form for computing By the most impsrt,a! Of ne
unavoidable errors II observation from those diresty
curves nre united, modulus by which the conducting
power may be expressd In this WY moving cold
rent the polar regions seeking tue BOTTOM oeing
the denser capped BY overow Of the warmer
water you would expect 10 dnd just such those
which hfst resulted from the observations Of JAWS aud
were ccuhrued by George Bache and by hts successors
One feature 10 these rerul OF considerable interest," +
his that they were made ny officers having no special
ny pOthesis collecting data from which hypotheses
might be made, confirmed refuted, fully convinced.
doutt that laS would come OUT Of fithfu results but
not particularly Interested in the form which il might
IanOrerS,
wneo discussing these results TO land them to- macy
tAgs but never more than for their strict
lime and hgsin ih,s Law rad been repeated when Lieut.
craven presented his winter results with some dis
coursgeuent that they were SO much less ar than
mex diagram gives nearly the same tempo sture from
me soihce Gown 70 loO 10 oomf we reflect that AZ
ths c",dsr a. &c s s,u ot IMPLY o'onns ~
su rs sinx Us sIey arc coSi.a.
90 10 some OF Lieut. Mantle results there we're trreyu
OF he stream and eveo temporary shifting Of the upper
sn II w . s.,ae WIN Hspscs 70 eaca o.nef.
arss tie navsasor- would have encoantorei
many wv - ~ suu u". VII su M le"au.
vations Of psossor Forbes and Qaesaet for tbs de-
90 ~ ssi , =, ~. =. III are t sas
e. N s, more Sonaosnes wi oe ,aapirea ~ then;
wy ul'ue .. .ne ease l' NUN Isger IN 81 mat pre-
ntu " me Iesnis % '1e ooass survey o.n 1913 enc
sauSo u ue huau u.euuu ~ luS lseI !ap.',s
u Changes OF tenpcstuss T. thus eieary manifesto
uea c1sse - taa ~n.cn os'onss 20 ppssa
.se aIa 'a &c
=. uss.an !. nss ,ne saAe isa. ICES OF
ne .ssscai s,asns ne aaa sne sn ~ casse ks
a. w .. sx'n o. cecuMetence, as 'ne o;aer ana
put sow ana pesses Gown 70 cepta o. some three Or
,at. ~ as.on W. o,v ~ ou NV; Maau wu ~
With a vertical Straight line, giving section whi:h
M ss wnn ~. o.n.s ~ nav wy gsn.e
a lug ns u Nv ' s
curve mas tessneo sne c"la waer. INV .n.S
ium Of empers,u sv c"ndncsn nor OUGHT we and
such in 'he moving mass OF gulf water which must cool
- ~ S ~ ~ w. o'U.o . ~ ,sS. .n' sa" =;
snother The IN, one which n saw In the nshnre dis
!; IN thoss nrc ,Sics.nod .rs ,hs 10 o rt y
eea baI- ,no 90 r. tht a ~ o -. =, ~ - ,h
T. ~ he y. " . 'e
that Size. and Is marked cSey as they overrun tho polar
in 49, oncar Wy s',Snnr. q; nanaI $3.50 4 - ths
easy 70 rec the dvisions Of the water serunize it
~ dm,t y ~ uaan0 INC nnA w snA1i nnu
TN S s - ~ ~ o .; ~. T., .ho ..,,. RI
ss o' IN " yPe cuevo 10 nas IL tug s aies " 10
Ia el, ,esea prog ,ae protecting part, OF sonedc, -
c nssv c.nso ~ sne .yps cve ,nsoose from sns
oten Drawn from previous suca Is u Is pre-.
r. Gu - .ne m LAC N aooa oy
These Tyre curves arc varlously nodded aud tusre
ono!s ~nicr socm - ccl,sn puts =. nc s.rosu
qu,s o. nea pos,ons ous ~ncn u T icss Rsn
es' - e.. ~ on ~ 1 ". no .n1 vs ~
easy an . sCu, anu LAW sumciea'y u"e upon
'As rrcsod ms ~ cc,s,o- +ho gross .ocon
A. PIoceco neA% 70 co9saoer VIE. tne cross scc.on o.
I 20 a. ny H. rS,' IT, S
tne o,agram 9, INC SAVOY HOOK secuon: ina aeep
"a wncn snc warm ~atcr hes WIa itssaIge pro
~ nns l.no, anu snos sr ono .ow ,lus
oosan, alo suino'cnsis A. Ac Anc Su.vos sno~
S as cs W leave :nose near .ho surface.
ne NOS " .usss Is aue sulusu cusage "
"Feau,c rMcn IN Yen u,,os ilses so%e oes ~
30 suddenly hat IN the diagan Of thi between the
as Leu1 nscnc calco ~ u Is almost sor.,cs
mus sams Iorm presents lscI 70 .ne s.ealest ooP.n %
the sounoings hamey lour nun areo Lannon's, th;uen
t~eny Sssreea IL atty Miles ieass seven
o1Snes "a my Mies 50 Pcriecay us0ocs IN
al the curves tnat it' ac'crmiraMon upon any
one woa,o pe pronounceo fatsssory Maen - Is Iecoi-
acsed tbat the ooselvsuon o. eaco deph an inas-
pendent me having no ipn betweeh taa' ao1ve
ana t9at below ~ tho induction Is complee Inc Owl
nov o. .pe Sun wa.er Is dsu9cy sncwn ~ .us curves
=. ano ~ Aaao~s, every phns 9srg "ouve Tug .1u.
petature OF % eeg IN tns rcction ~ tnese 9ep,hs
rassng rom we Se6cy Hook SECTION 70 va. on capc
any 10 .nat Oh SsP ueeIy' .ne saae resu. snoSs
So 4 ~ 40 eyu W., 90 :. wo.c, naius .Se
ha,e escr,,i tbs cI,mse oS bu .rd snS