The impact of in-canopy wind profile formulations on heat flux estimation using the remote sensing-based two-source model for an open orchard canopy in southern Italy

The basic problem (4) for the arbitrary assumed value of boundary heat flux q ( x , t ) and the additional problems (20) associated with the sequential function specification

XRF analysis of third instar wing imaginal discs, showing distribution of copper (left panel), zinc (middle panel) and iron (right panel). Distribution is shown as a heat map with

Radiometric-based sensible heat flux H rae along transects over the three main land use classes, processed using aircraft surface temperature and net radiation data, com- pared with

Correspondingly, the P-M model with J-D bulk canopy resistance slightly underestimated the latent heat flux throughout the maize growing season, but overestimated the latent heat

Thus, in the lower third of the CBL the turbulent heat flux is posi- tively correlated with water vapour mixing ratio, i.e., the upward directed turbulent heat flux originated in

of snow ablation including net solar radiation, turbulent flux exchange of sensible and latent heat and the e ff ect of local advection of sensible heat. We investigate the ap-

Instantaneous net radiation map is shown in Figure 3, NDVI map is in Figure 4, surface temperature map is in Figure 5, soil heat flux map is in Figure 6, sensible heat

K EYWORDS : Heat island, Topographic flow, Urban canopy model, Urban soil model, Anthropogenic heat flux..