Consider a general case where soil moisture may limit the surface specific humidity. In this case actual latent heat can be modeled using Equation (8.5.12). Consider two cases: 1) a saturated soil as mentioned above; and 2) a water-limited case (volumetric soil moisture is 80% of the field capacity) where the multiplicative reduction factor is given by Equation (8.3.20). Use an appropriate model to compute the latent heat flux using the above measurements for each of these cases. How do the values of the fluxes between the water-limited case and the saturated soil case compare