Re-analyzing the data published by the Berlin and Düsseldorf ether-drift experiments, we have found a clean non-zero daily average for the amplitude of the signal. The two experimental values, A 0 ∼ (10.5 ± 1.3) · 10 −16 and A 0 ∼ (12.1 ± 2.2) · 10 −16 respectively, are entirely consistent with the theoretical prediction (9.7 ± 3.5) · 10 −16 that is obtained once the Robertson-Mansouri-Sexl anisotropy parameter is expressed in terms of N vacuum , the effective vacuum refractive index that one would get, for an apparatus placed on the Earth's surface, in a flat-space picture of gravity .