INVESTIGATING CUMULUS CLOUD FORMATION
by Walter
Sanford
Planetarium Teacher, Fairfax County
Public Schools
BACKGROUND
Cumulus clouds are caused
by convection, during which a parcel of warm, moist air rises and cools
until the air temperature equals the dew point temperature and invisible
water vapor condenses to become liquid cloud droplets or solid ice
crystals. When air rises, it cools at a lapse rate of approximately 10
degrees Celsius per kilometer. The dew point temperature also decreases,
but at the lower lapse rate of 1.7 degrees Celsius per kilometer. To
predict the approximate height at which cumulus clouds will form, known as
the Convective Condensation Level (CCL), write an algebraic equation to
calculate the altitude at which the air temperature equals the dew point
temperature.
Solution:
A = Tg - DPg / 8.3
where:
A = CCL (in kilometers)
Tg = air temperature at ground level (in degrees Celsius)
DPg = dew point temperature at ground level (in degrees
Celsius)
ACTIVITY EXTENSION
Use the Texas Instruments
TI-82 (or TI-83) graphing calculator to plot a graph that can be used
to determine the CCL (given the air temperature and dew point temperature
at ground level).
PROCEDURE
- Randomly select five pairs of ground level air temperatures and
dew point temperatures, e.g., 30 & 25, 30 & 20, 30 & 15, 30 & 10, and 30 &
5. Use the algebraic equation (above) to solve for the CCL. On
the graphing calculator, enter the resulting altitudes as List 2 (L2).
- Using the same five pairs of numbers (as in Step 1 above), calculate
the ground level Dew Point Depression (DPD), e.g., 30 - 25 = 5, 30 - 20 =
10, 30 - 15 = 15, 30 - 10 = 20, and 30 - 5 = 25. On the graphing
calculator, enter the ground level DPDs in List 1 (L1); be sure to enter
the DPDs in the same order as List 2 (L2).
- Using L1 as the "x" value, and L2 as the "y" value, graph the data.
(For step-by-step instructions, refer to TI-83
Help.)
- Use the "TRACE" function to determine the CCL for other combinations
of ground level air temperature and dew point temperature. Note the X and
Y coordinates at the bottom of the screen--the "Y" value is the CCL (in
km) for a given DPD (X value).
Copyright © 1996-2010 by Walter Sanford. All rights
reserved.
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