Lake breeze structure
Seagal et al. 1997
Scaling
arguments:
•Cooling
over water weaker than heating over land
•Increased
sensible heat flux over land increases wind speed
•W/L>>1,
wind speed weak
•W/L<<1,
wind speed increased 60% compared to W=L
•Lake
half width should be wider
than CBL depth to see lake breeze distinct from convective
eddies