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4000

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MIDWAY

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LL
SOLDIER'S FIELD
(MEIGS)

Fig. i102—Vertical temperature cross section over Chicago, December 16, 1968

limit mixing. Profiles at the other airports were simi-

lar. (The SOz2 sensor on the flight package uses the
David conductivity method. It is unable to distin-

guish between SOz and COs; a scrubber is used to

eliminate the SOz before the conductivity is measured.
The CO. contribution is then subtracted from the COz

plus SO» reading. In Figure 101, the periods when the
scrubber was in operation are shown.)
Several other flights have also been made using a

very simple thermistor bridge combination furnished

by the National Air Pollution Control Administration.
This package has been flown both on a helicopter and

on a light airplane. The thermistor, inside an aluminum radiator shield, was mounted at the forward end

of the landing skid of the helicopter or on a strut of
the airplane. The thermistor resistance was measured
by manually nulling a Wheatstone bridge having the

thermistor as one resistance element and a 10-turn
potentiometer as another. Temperatures were then determined from a resistance vs. temperature calibration chart. Heights were taken directly from the aircraft altimeter.

The first of these flights was made on December 16,
1968, when vertical temperature profiles were observed
over Meigs (lakefront) and Midway (urban) Airports
in Chicago and over Argonne(rural), using a Chicago
Fire Department helicopter.
Figure 102 shows the variation of temperature with

height between Meigs Airport on the lakefront and

Argonne. The three profiles are very similar, showing
adiabatic lapse rates up to a strong inversion layer at

about 2000 ft. Some of the horizontal differences may
be due to the fact that the sounding at Meigs was
made at 1000 CST, at Midway at 1015, and at 1100

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