M. Davis et al., COMPARISON OF VELOCITY AND GRAVITY FIELDS - THE MARK-III TULLY-FISHERCATALOG VERSUS THE IRAS-1.2 JY SURVEY, The Astrophysical journal, 473(1), 1996, pp. 22-41
We consider a measure of the peculiar velocity held derived from the M
ark III compilation of 2900 spiral galaxies (Willick et al.), using an
analysis method that is substantially free of bias (Nusser & Davis).
We expand the velocity held in a set of orthogonal, smooth modes, redu
cing the data to a set of 56 coefficients fitted to a maximum redshift
of 6000 km s(-1), and maximum spherical harmonic of l = 3. The radial
resolution of the modes degrades with redshift, from 800 km s(-1) loc
ally to 3000 km s(-1) at 4000 km s(-1) redshift. Equivalent mode coeff
icients can be computed for the gravity held derived from any whole-sk
y redshift catalog of galaxies, such as the IRAS 1.2 Jy survey (Fisher
et al.). Given the coefficients of the expansions, one can compare th
e velocity and gravity fields on a galaxy-by-galaxy basis, or on a mod
e-by-mode basis. Detailed comparison shows the two independent fields
to be remarkably aligned in general. There are, however, systematic di
screpancies in the fields that lead to considerable coherence in the r
esiduals between them. These residuals take the form of a dipole held
in the Local Group (LG) frame that grows with distance; it is not cons
istent with a bulk flow residual. We perform a likelihood analysis in
the mode-mode comparison to determine which value of beta = Omega(0.6)
/b for the IRAS gravity held is the best fit to the Mark III velocity
held, considering the errors and covariance in both the velocity and g
ravity coefficients. We find that the most likely value lies in the ra
nge beta = 0.4-0.6. However, in contrast with results we obtain using
simulated galaxy catalogs, the chi(2) per degree of freedom for the fi
t is well in excess of unity, primarily because of the coherent dipole
residuals at cz greater than or similar to 3000 km s(-1). Thus, despi
te the general alignment of the Mark III velocity and IRAS gravity fie
lds, they do not agree in detail, precluding a firm determination of b
eta from these data sets at present. The method is capable of measurin
g beta to an accuracy of 10%, but without understanding these systemat
ic discrepancies, we cannot infer a value of beta from these data.