|Annu. Rev. Astron. Astrophys. 1994. 32:
Copyright © 1994 by Annual Reviews. All rights reserved
2.3. The Correlation Function
It is conventional in CMB work to expand the temperature fluctuations in spherical harmonics
and work in terms of the multipole moments am. One can define the sky correlation function
where the average is taken over the (observed) sky with the separation angle 21 held fixed. Using the properties of Ym the correlation function Csky(21) (hereafter we will drop the subscript "sky") is
where we have introduced the rotationally symmetric quantity a2 m |am|2. The a2 are not to be confused with (2 + 1) C (see later) which is often used to define the power spectrum of fluctuations in a Gaussian theory. At this point we have made no assumption about the underlying theory of fluctuations or the model of structure formation - the a2 are purely measured quantities on the sky. [Note that other authors' definitions of various quantities can differ from ours by 4, (2 + 1), or similar factors.] The COBE team (C. Bennett et al 1992, Kogut et al 1993, Fixsen et al 1994, Bennett et al 1994) quote results for the first two moments, i.e. a T0 / (4) for = 1, 2,
A common way of comparing theory and experiment is through the am. Of course an actual measurement of a temperature difference on the sky involves finite resolution and specific measurement strategies modifying Equation 5. These are usually included in the theoretically predicted correlation function through a window or filter function, W, described in Section 4.2.