We discuss the properties of the solar background signal as observed in hig
h-quality, l - v power and phase difference spectra of the continuum (C), v
elocity Oil, and line intensity (I) fluctuations of the Ni I 6768 Angstrom
line. These spectra were generated from high-resolution images acquired by
the Michelson Doppler Imager on board SOHO.
We confirm that the background signal in the velocity power spectra can be
reproduced by a composite model with two quasi-stationary components, descr
ibing large-scale and small-scale convective motions, and a periodic compon
ent. The line and continuum intensity power spectra require additional quas
i-stationary and periodic components. The extra quasi-stationary component
dominates the intensity and continuum background signals over the spectral
region where the I-V phase difference spectra show essentially constant neg
ative phase difference: i.e., below and in between the p-mode ridges (calle
d the plateau-interridge regime by Deubner et al.). Since the I-V phase bet
ween the p-mode ridges is not random, the solar background beneath the p-mo
des must be considered as coherent. We thus speculate that the negative pha
se regime may be the manifestation of a correlated background. Such a backg
round has been proposed to explain the opposite sense of the asymmetries of
the p-mode line profiles in velocity and brightness oscillations.