Cyclic Daily Valley Fog Aggregation

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Presentation transcript:

Cyclic Daily Valley Fog Aggregation Addien Wray

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

Movie!

(Run code using: valley_fog_aggregation.m)