Flow visualization by PIV method
Surface temperature difference between 1/5 and 1/50 scale models
Heat storage term becomes larger with wind veclocity deceasing
Typiecal diurnal chnage of energy balance
Drag coefficients of 1/5 and 1/50 scale models : siginificantly dependent on wind direction
Energy imbalance of eddy correlation method obsevbed by scale model experiments
Cross over phenomena of temperaure profile between scale model and fetch region)