Santa Fe new Mexican. [volume] (Santa Fe, N.M.) 1898-1951, 1900-05-30
THE SUPERB CLIMATE
Santa Fe Has Fine Summers and
Moderate Winters with Equable
Temperature.
NEARLY ALWAYS PLEASANT
The Salubrious Atmosphere Of the Terri,
tory and Reasons Why the Climate Is
Healthful and the Country Chosen
for Sanitariums.

A knowledge of the contour OF New
Mexico in relation to the surrounding
country is necessary to clearly nder-
stand the cause of it's climatic advant-
ages, that are not possessed by any
other part of the United States. A
study of the Rocky mountain region re-
yeals the fact that the great chain
from the far north is broken in its con-
tinuity as it leaves Colorado. In New
Mexico there are smaller ranges with
here and there lofty peaks with timp-
cred slopes and barren crowns to re-
lieye the clouds of moisture. From
them incline fertile valleys and grassy
upland plains to the gulf region until
when the southern border Is reached,
there are no mountains between New
Mexico and the southern water. Three
fourths of this territory has an altitude
of 5000 feet. At the southern border
the valleys have dropped to from 5000
to 1000 feet, while the Santa Fe valley,
at the capital city, has an altitude OF
6,967 feet at the plaza.
A country Of such varied attitudes
must nave some variety in climate, but
the variation is In degrees Of tempera-
ture mainly, for in general h climate
of New Mexico Is dry and salubrious.
The rainfall is principally confined to
showers in the summer, with little rain
or snow in the winter. except In the
northern part Of the territory.
Near the extreme southern line, In
the Sacramento mountains, a lofty
peak is the first considerable elevation
met with, as the moisture-laden gull
clouds drift to the northwest, and this
precipi iates rain to greater extent thar
any other mountain. the rainfall there
having in exceptional seasons been es.
timated at 4S inches. But over h ter
ritory the normal precipitation ranges
from s to IS inches, according to eleva'
ton.
, COMPARATIVE TEMPERATURE.
The southern valleys are. of course
! the warmest portions Of New Mexico II
the summer, but the hottest are pleas
; anter in midsummer than the east. be
cause the air is dry. rapidly absorbs tn
D dampness of the skin and has a cooling
t effect. The weather Is never oppressive
e the nights are always cool enough t
: sleep under cover and generally unde
a blanket.
: Santa Fe, being up out Of the grea
: valley of the territory, is especial,
e blessed as to summer temperature. tn
e highest record by the thermometer !
It this city in tw~enty-six years was So de
d grees in 1873, an extreme rarely ap
G preached. In the last ten years 81 wa
the highest absolute temperature.
Y should be borne in mind that in a dr.
It climate the record of the metallic ther
mometer does not indicate the real TEN
pe%rature felt by a human body, whic
is cooled by the drying effect of the all
It has been demonstrated that a TEN
p~erature of 80 at Santa Fe is not NOR
oppressive and heating than u ats
Louis, or at any place with a humid eli
mate.
i The following table was made u
from reports of the climate and Gro
service of the weather bureau, an
9 gives a general idea Of the relative ir
tensity of heat as indicated by the M
. tallic thermometer: