A wind blowing from left to right across the mountain
is traced by a leaf as a marker. The initial conditions of the atmosphere
at the base of the mountain on the left side are represented
by the leaf placement on the vapor pressure/temperature graph. The
conditions corresponding to the initial leaf placement
of the simulation when the graphs first appear will not cause a
temperature difference between the initial and final
conditions.
A. Run the simulation for this case and use this as a reference for future observations.
B. Next experiment with various
initial positions of the leaf on the vapor pressure/temperature graph in
order to achieve a 5-5.5 degree Celsius difference between the temperatures
ground on either side of the mountain.
1. What was your plan for finding the "correct" initial leaf position?
2. How does the leaf path on the vapor pressure/temperature
graph for the reference case compare with the path where the 5-5.5 degree
Celsius temperature difference occurs? What do you think is happening?
3. How does the path on the altitude/temperature
graph for the reference case compare with the path where the 5-5.5 degree
C temperature difference occurs? Can you suggest a reason for the differences?
4. Watch both graphs simultaneously during conditions
when a cloud forms. What relationship between the two curves do you observe?
5. If a cloud formed but no rain fell, could a temperature
difference ever occur between the windward and leeward sides of the mountain?
Why or why not?