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 1t.
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 10y the surrounding
cooler air.
When the ascending current reaches
a stratum of equal temperature. 1t
ceases " move upward, but being
pressed upon from beneath, is diffused
horizontally In every direction. Be
coming gradually cooler, it sinks and
again becomes a part Of the horizontal
current moving in the direction of the
heated portion. The descending cur
rent reaches the earth somewhat be-
You'd the tropics; only u part. however,
returns TO the heated regions as above
described: the remainder continues Ia
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 at rest and its
surface uniform, the currents would
follow the meridian To and from the
| equator; but the rotary motion of the
earth rnuScs the currents as they APP
pronch the equator 10 turn toward the
west Therefore. In the Northern
Hemisphere they are northrastcrly
winds, AMI In the southern. southeast
erly. The return currents, on the con.
'rary. being DETECTED toward the east.
become sOuthw">terly winds in the
Northern Hemisphere, and northwest.
crly In the southern.
There are numerous notifications in
the direction of these general eur.
rents. caused by the direction of noun.
tain ranges, relative position of the
land masses AMI the oceans. etc. For
instance, the polar currents starting
In the far North and advancing to.
ward the equator. fall more AMI more
under the influence of the earth's rO-
| tnry motion AMI tend everywhere to
become northeast winds: hut the Rocky
Mountains defect their course and
turn them toward the southeast: hence
the cold dry winds Of the Atlantic
seaboard are from the northwest.
The prevailing winds near the sea.
board are known rs land AMI sea
brccZcs. This phenomenon Is more
| strongly marked In the tropical zone
ana 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
| Is much higher than over the water.
| Soon after sunrise a breeze begins ~
set IN from the sea AMI continues with
increasing force until about , O'Clock
when the difference Is greater. Ii
then gradually decreases until about
shutdown when there Is u perfect calm
for an hour ~ 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 Is the coolest. 4
calm then prevails which Is soon re-
placed by the sea-brceZe. \ similar
breeze occurs on the shores of great
lakes and NJ the foot Of high noun
tains. The inclined slopes of noun.
tains have, during the day, u higher
temperature than the atmosphere in
corresponding attitudes, hence become
the natural channel Tor the ascending
| currents from the plains below. Dur.
ing the hottest part of the day. breezes
ascend the valleys toward the noun,
tains, --Nomal Instructor.