“…We conducted a series of campaigns in successive summers at White Mountain and then for two successive years at the South Pole which is also a high and very dry site with a very stable and relatively small atmospheric signal. We published a series of papers on the theory, observations, and interpretation leading to a much improved set of measurements at long wavelengths ͑Danese and de Zotti, 1977Zotti, , 1982Smoot et al, 1983aSmoot et al, , 1983bSmoot et al, , 1984Smoot et al, , 1987Smoot et al, , 1988Mather et al, 1994͒. The few additional observations that have tried to improve on these measurements have been generally balloon-borne versions with the same basic concept but above much more of the atmospheric signal.…”