1. Cyclic Daily Valley Fog Aggregation
Addien Wray

2. MATLAB Interpretation
Valley Fog Feature
MATLAB Interpretation
Cyclic heating/cooling over a day
Temperature of surface α sin(t)
Air temperature decreases
with altitude above ground
Linear interpolation of temperature
at surface and max Y (top of atm)
Daily temperature swing and average
differ for valley and peak
Assigned as constants,
dependent on elevation
Water capacity of air α Temp
Probability of particle
formation/loss α Temp at Y

3. Movie!

4. (Run code using: valley_fog_aggregation.m)