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Introduction
The University of North Dakota's
citation aircraft can measure a cloud property known as liquid water content
(LWC). It is defined as the mass of liquid water in a given volume
of air. It is measured by an instrument called a King probe.
Figure 1. The King probe is typically located under the right
wing.
The probe is manufactured
by Particle Measuring Systems, Inc. in Boulder Colorado. It consists
of a long, thin metal coil 4. 0 cm in length, 2.0 cm of it is the master
coil exposed to the air, and .187 cm in diameter. The coil is connected
to a circuit and a voltage is supplied to the coil at a constant temperature
of about 185 degrees Celcius. When water droplets come in contact
with the coil they evaporate due to the high temperature of the coil.
The latent heat is to evaporate the water is supplied by the coil.
The coil is controlled to maintain a constant temperature throughout this
process by an electric circuit. This voltage can be measured and
is proportional to the energy provided to the water droplets. This
energy quantity tells how much liquid water is in cloud.
The power supplied to keep
the coil at a constant temperature is made up of the sum of two components.
Not only is power supplied due to the evaporation of water but it is also
supplied because energy is transferred to the surrounding air molecules
because of the difference in temperature between the air and the coil.
The liquid water content is calculated by using measured values of the
voltage, air speed, ambient air temperature, and pressure in an equation
and solving for the LWC. This equation is shown on the
equations
page.
The King probe can accurately
measure droplets in the range between 10 and 40 micrometers in diameter,
according to "The Drop-Size Response of the CSIRO Liquid Water Probe" by
Biter, Dye, Huffman, and King. There is an average error of about
five percent for droplets smaller than 10 micrometers because the smallest
droplets tend to follow the streamlines of air around the coil. For
droplets of diameter greater than 40 micrometers the error gradually increases
to about 50% for droplets of about 150 micrometers in diameter.
The data collected by the
King probe is used in projects to study cloud properties, such as aircraft
icing. Most recently data from the King probe has been used to compare
with data from the department's microwave radiometer, which measures liquid
water path.
Figure 2. Close-up picture of the King probe.
Continue to Equations page
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