{"newspaper_name": "The New York herald.", "edition": "01", "page": "p2", "byline": ""}
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INTERESTING FACTs-CLIMAToLoaY.- sud
)ect formed very interesting portion OF one OF PrG
lessor Lyes recent lectures before the Lowell nsttu


having regard to the laws attending the distribution


heat the surface of the earh to the consider


hon OF Bufons great error the subject of the en


equality Of corresponding zones, or, Of the SAM
parallels east and west, whereas in truth they oc
differ prodigiously Humbodts doctrine of the ceothe
NAL line above which, few feet or even inches,
low the surface, the ground never thaws, was e
planned clearly, well its excessive irregularty II
low pressure in America, Gas shown by the colored ln
drawn upon an extensive map mercator scale
hoIted during the lscture) being ascrbed to TIL
being laid down general rule that any land heyonl
oo' parallel must always exercise chilling effect q
the places next south of discriminating Of course, as
situation further removed though in some d. gree
even TO the tropics. The plainly seen in hI
extensive accumuations OF snow which such circun
stance allowed, as well as ITS s.cindinS the warm
the higher latudes, to milden the ctimate-as, fuI
instance the northern parts of Norway and Swede


where from the coast of Labrador that Iine sweeps


wards u II fifteen degrees towards the pole There we
other corresponding lines at different parallels ais
depicted on large maps, the fexures OF which we n
ns - tbsy ue were artbsr ns


the polar accumuations, which, like an immens
mounain, extended their chilling effects to
distance around In this lecture the relative situation
the cities Of New York in America and of old York
England were quite happily contrasted by Professor


Ia huustrauon OF his previous remarks. The same
thermal line, seems, passes through both though tn
latter be deg to the north Of our sister metropolis Blu
the difference in climate, owing to influences before
mentioned, was found to be really very great sine
at opposite seasons was full eighty degrees frequs
gong through much Of this in very lew days, that q


the elder city scarcely ever exceeded sixteen degree
IRON winter to summer.-year after ye&r OF the me
OF Manhattan then most truly may IL he said they hav
the summer OF Rome and the winter Of Copennagen 81
mighty indebted are we on the American coast to th{
provinces, to Greenland ice and opposition OF Gu
Streams and Ocean fogs.-Bosfon Transcript, Dec. J.