Chicago eagle. [volume] (Chicago, Ill.) 1889-19??, 1901-05-04
TAX Them TO DEATH.
That Is the Policy Of the Drainage
Trustees with Respect to
Chicago People.
Money Must Be Raised for the Con.
tractors and the People
Must Pay It.
The Carpet Baggers Who Are Behind the
Scheme Own No Property
At All.
But the People Who Do Must Pay to Keep
These Favorites in Pin
Money.

stove. Is replaced by the surrounding
cooler mir.
When the ascending current reaches
a stratum Of equal temperature, II
ceases 10 move upward, but being
pressed upon from beneath, Is diffused
horizontally In every direction. Be-
coming gradually cooler, 1t sinks and
again becomes part of the horizontal
current moving In the direction Of the
heated portion. The descending cur
rent reaches the earth somewhat be-
yOnd the tropics; only a part. however,
returns to the heated regions as above
described; the remainder continues IN
the direction Of the poles. This lat
ter current Is always more or less Ia
contact with the current setting to.
ward the zone of greatest heat, AMI the
conflicts between these two struggling
for supremacy, produce frequent
storms.
Ii the earth were ut rest and Its
surface uniform. the currents would
follow the meridian to AMI from the
equator; but the rotary motion Of the
earth causes the currents as they ap-
prOnch the equator to turn toward the
west. Therefore, In the Northern
Hemisphere they are northeasterly
winds, and In the southern, southeast.
erly. The return currents, on the con-
trary. being DETECTED toward the east,
become southwesterly winds in the
Northern Hemisphere. and northwest.
crly In the southern.
There are numerous notifications In
the direction Of these general cur.
rents. caused by the direction of noun.
tain ranges, relative position of the
land masses and the oceans, etc. For
instance. the polar currents starting
In the far North and advancing 10.
ward the equator. fall more and more
under the influence Of the earth's 70.
tnry motion and tend everywhere to
become northeast winds: hut the Rocky
Mountains defect their course aud
turn them toward the southeast; hence
the cold dry winds Of the Atlantic
seabOard are from the northwest.
The prevailing winds near the sen.
board are known as land and sea
breezes. This phenomenon Is more
strongly marked In the tropical zone
and In the summer ATTITUDES OF the
temperate zones. because of the great.
er inequality In the heating of the land
and sea by day and by night. During
the day the temperature over the land
IL much higher than over the water.
Soon after sunrise u breeze begins to
set In from the sea AMI continues with
increasing force until about 3 o'clock
when the difference IL greater. II
then gradually decreases until about
shutdown when there Is a perfect calm
for an hour or more. Radiation caus.
Ing the land to become cooler than the
sea, u breeze from the former sets In
and continues until Just before day.
break when the land Ia the coolest. A
calm then prevails which IL soon re.
placed by the sea.brceze. 4 similar
breeze occurs on the shores Of great
lakes and at the foot Of high noun.
tains. The inclined slopes OF noun.
tains have, during the day, a higher
temperature than the atmosphere In
corresponding attitudes, hence become
the natural channel for the ascending
currents from the plains below. Dur.
ing the hottest part of the day. breezes
ascend the valleys toward the noun.
NOmal Instructor.