astrolollo said:
Hi everyone
Given the definition of ##C_{l}##, ##C_{l}=\frac{1}{2l+1} \sum a_{l,m} Y_{l,m}##, I was wondering how it is possible to measure the ##C_{l}##s in practice. How does one compute this quantity, having a map of the temperature anisotropies of the CMB?
To expand a little bit upon what Orodruin said, the first step is to take a spherical harmonic transform:
a_{\ell m} = \int Y_{\ell m}(\theta, \phi) T(\theta, \phi) sin(\theta) d\theta d\phi
Here ##T(\theta, \phi)## is the CMB temperature in different directions on the sky. There are various mathematical tricks used to make this integral efficient to compute on a computer (a common library used for this is Healpix).
The power spectrum is then the variance of the amplitude at a given ##\ell##. Each ##Y_{\ell m}## can be thought of as a wave on the surface of a sphere, with the wavelength given by ##\ell## and the direction given by ##m##. Each ##a_{\ell m}##, then, is the amplitude of the wave with wavelength ##\ell## and direction ##m##. To get the power spectrum, we take the variance of the wave amplitudes of each direction at a given wavelength:
C_\ell = {1 \over 2\ell + 1} |a_{\ell m}|^2
Here the factor of ##a/(2\ell + 1)## comes from the fact that ##\ell## and ##m## are integers, with ##\ell \ge 0## and ##-\ell \le m \le \ell##. For example, if ##\ell = 2##, then ##m = {-2, -1, 0, 1, 2}##.
There are lots of other complications that come in from the fact that there is stuff between us and the CMB, so that we don't have a perfectly-clean full-sky map. Various techniques are used to extract the CMB signal, but I think I'll stop here for now.
Does this answer your question? Did you have any other concerns?