Abstract
The possibility that the day-to-day changes in absorption at Slough, Swansea, and Freiburg are identical is examined statistically. After allowing for known sources of error, it is considered that the residual differences in summer months are too small to bo significant, but that it is probable that real differences occur in winter. In both cases the minimum probable correlation for the Swansea-Slough comparison is very high—about 0.92.
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