Milford chronicle., 1906-04-27
CLIMATE OF The UPPER AIR
Variation OF Temperature In Atmos-
phere at Great Height.

Variation OF Temperature In AtmOs-
phere at Great Height.
That at great heights. 10000 or 10000
feet the seasons occur at different
times Of the year from these on the
surface Of the earth jyst below appears
from numerous measurements of tenn
perature taken with sounding bal
looms" or small captive balloons con-
tanning automatically Registering in
struments.
The fact that midsummer comes in
October In the upper air and nidwin-
ter in April appears to have an i'm
portant influence on the weather of
these months, as is noted in an article
In Ciel ct Terre, distracted in Cosmos.
The author first notes that the upper
air temperatures measured by the
method referred to above are surprls-
ingly low. He writes:
"Facts regarding thermic conditions
in the upper regions Of the atmosphere
are always Of interest. Data collected
on this point several years ago by
means of sounding balloons caused
some astOnishment. but nevertheless
they do not appear so remarkable when
we compare them with facts obtain
ed more recently, since aerOstats and
perfected devices have made it pOssi-
ble for us to penetrate to still loftier
elevations.
ION Dec >, 1901. balloon sent up
at Trappes. near Versailles, by Teis-
serene de Bort reached the height Of
4G.904 feet At tbs great height the
temperature was 90 degrees T. In the /
same December piece of apparatus |
sent up by Mr.. Rotch at st. Louis reg |
lstered 122 degrees F. at 4S544 feet
These figures. which are actual rec
ords, have now been exceeded, as we
shall see, at least so far as the Eu-
rOpean continent goes.
I'm the intercollegiate Zeitschrift
for July last r. Nimfuhr announces the
temperature registered on two sound
ing balloons sent up from Vienna on
March and April 4, 1905. The mini
ma recorded In these ascensions were,
on March 2, 121 degrees F. at 31,S72
feet, and on April 4, Ill degrees T. at
36,113 feet These represent up to the
present day the extreme figures re-
corded in Europe.
at is important to note in this re-
gard that in the elevated layers of the
atmosphere the fluctuation of the tenn
perature undergoes a well marked an
nual variation which, however is not
parallel to that which is familiar to us
on the lower levels. The seasons in the
upper air are late, the greatest cold oe-
curing toward spring the beginning
Of April and midsummer about the be-
ginning of October
"This peculiarity has some influence
on the condition Of the atmospheric
strata. The prOverbial variability Of
the weather in spring results largely
from the fact that then the atmosphere 1
Is generally in a state of unstable
equilibrium. due to the cOldness and
excessive weight Of the up
per layers in relation to the lower, .
which, being already somewhat warm. .
ar, are lighter. |
"Now we know that the equilibrium ]
Df a mass of air is most stable when 7
he layers that are relatively warm [
md light are above the colder ones. (
This condition is most often realized in I
autumn for the reason indicated above, S
md the weather then is less variable /
Sometimes the upper air also under l
soes extraordinary thermal variations G
n the course of day or two t
During the same lapse Of time the v
distribution of barometric pressure and O
on the earth's surface re- &
mains sensibly the same. Literary
Digest.