Components of the surface energy balance on a summer day in Pitt Meadows, Canada (49 ° N), above an irrigated agricultural land (graph from Stull, 1988; data from Oke, 1978) The relationship between sensible heat flux and latent heat flux is called Bowen's relationship
β = Qh / Qe
and it depends on the humidity available in the soil, the type of soil and the ground cover
(type of vegetation etc)
Ground Cover - Typical values of Bowen's relationship
1:100 Scale dwg file (meters) Conversion from meters to feet: a fast and fairly accurate system consists in scaling the drawing by multiplying the value of the unit of measurement in meters by 3.281
