Some experiments to measure concentration fluctuations downwind of two trac
er sources in the atmospheric surface layer are described and the results p
resented. Fast response detectors were used. The sources were at a height o
f 4 m and the experiments were restricted to short ranges where the how and
turbulence can be assumed to be approximately homogeneous for the purpose
of predicting the dispersion. The results are analysed to show the downwind
evolution of the intensity of fluctuations for each source separately and
to show how the correlation between the concentrations from the two sources
varies with downwind distance and source separation. The variation of the
intensity of fluctuations and the correlation with averaging time is also e
xplored. Results support the idea of a universal behaviour when suitably sc
aled.