The dynamics of water and thermal conditions at soil surfaces are relatively complicated. First, they are scenario dependent. Multiple ambient factors, such as weather, soil properties, residue mulch, surface runoff, and additional field management practices can impact surface water and heat fluxes. For example, for a bare soil surface, evaporation follows the Penman model (Allen et al., 1998), while with surface mulching, either the mulch is impermeable to vapor flow (Ham & Kluitenberg, 1994), or vapor transfer within the mulch must be quantified to compute surface evaporation (Enrique et al., 1999;Findeling, Chanzy, & de Louvigny, 2003). Temperature at a bare soil surface can be determined using a surface energy balance. When surface runoff occurs, however, ponded water can exert direct influences on soil surface temperature, because liquid water has a relatively large heat capacity. Second, the time periods that ambient factors manifest their effects depend on the processes. For example, the variations of wind speed and surface temperature gradients can induce instantaneous effects on evaporation and sensible heat fluxes by altering the dominant