Testing the hypothesis on the relationship between aerodynamic roughness length and albedo using vegetation structure parameters

Surface albedo (α) and aerodynamic roughness length (z ₀), which partition surface net radiation into energy fluxes, are critical land surface properties for biosphere–atmosphere interactions and climate variability. Previous studies suggested that canopy structure parameters influence both α and z ₀; however, no field data have been reported to quantify their relationships. Here, we hypothesize that a functional relationship between α and z ₀ exists for a vegetated surface, since both land surface parameters can be conceptually related to the characteristics of canopy structure. We test this hypothesis by using the observed data collected from 50 site-years of field measurements from sites worldwide covering various vegetated surfaces. On the basis of these data, a negative linear relationship between α and log(z ₀) was found, which is related to the canopy structural parameter. We believe that our finding is a big step toward the estimation of z ₀ with high accuracy. This can be used, for example, in the parameterization of land properties and the observation of z ₀ using satellite remote sensing.