Air temperature measurements within a maize row canopy were carried out to investigate the horizontal and vertical variability of the mean air temperature. Attention was given to finding adequate scaling parameters of the within-canopy air temperature profiles under various atmo spheric stratification states. It appeared that in a narrow-row crop the horizontal mean air temperature can vary between 0.1 °C (night time) and 0.35 °C (daytime) from its spatial mean value. Exceptions can occur around noon under daytime situations when direct irradiation dominates and where the direct beam illuminates the within-row space of the canopy. Then differences to the spatial mean value of 1 °C or more can be observed. During daytime, the within-canopy temperature profiles scale well with the above-canopy temperature scale, T*, for 'constant' irradiation and wind speed regimes. During calm evenings, however, the rela tive within-canopy temperature profile scales very well with the within-canopy free convec tion temperature scale, 0*. It appeared that the within-row and across-row heat advection is of minor importance within dense row canopy.