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and Cosmology

Extragalactic Astronomy and Cosmology: An Introduction

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8. <strong>Cosmology</strong> III: The Cosmological Parameters<br />

346<br />

verification of the COBE measurements. In Fig. 8.30,<br />

sky maps by COBE <strong>and</strong> by WMAP are displayed. The<br />

dramatically improved angular resolution of the WMAP<br />

map is obvious. In addition, it can clearly be seen that<br />

both maps are very similar if one compares them at<br />

a common angular resolution. This comparison can be<br />

performed quantitatively by “blurring” the WMAP map<br />

to the COBE resolution using a smoothing algorithm.<br />

Since WMAP is not observing at exactly the same frequencies<br />

as COBE, it is necessary to interpolate between<br />

two frequencies in the WMAP maps to match the frequency<br />

of the COBE map. The comparison then shows<br />

that, when accounting for the noise, the two maps are<br />

completely identical, with the exception of a single location<br />

in the Galactic disk. This can be explained, e.g.,<br />

by a deviation of the spectral behavior of this source<br />

from the 2.73 K blackbody spectrum that was implicitly<br />

assumed for the aforementioned interpolation between<br />

two WMAP frequencies. The confirmation of the COBE<br />

measurements is indeed highly impressive.<br />

Fig. 8.30. Comparison of the CMB anisotropy measurements<br />

by COBE (top) <strong>and</strong> WMAP (bottom), after subtraction of<br />

the dipole originating from the motion of the Sun relative to<br />

the CMB rest-frame. The enormously improved angular resolution<br />

of WMAP is easily seen. Although these maps were<br />

recorded at different frequencies, the similarity in the temperature<br />

distribution is clearly visible <strong>and</strong> could be confirmed<br />

quantitatively. From this, the COBE results have, for the first<br />

time, been confirmed independently<br />

frequency range, using five (instead of three) frequencies;<br />

it has a much improved angular resolution (which<br />

is frequency-dependent; about 20 ′ , compared to ∼ 7 ◦<br />

for COBE), <strong>and</strong> in addition, WMAP is able to measure<br />

the polarization of the CMB. Results from the<br />

first year of observation with WMAP were published in<br />

2003. These excellent results confirmed our cosmological<br />

world model in such a way that we are now justified<br />

in calling it the st<strong>and</strong>ard model of cosmology. The most<br />

important results from WMAP will be discussed in the<br />

following.<br />

Comparison to COBE. Since WMAP is the first satellite<br />

after COBE to map the full sky in the relevant<br />

frequency range, its first year results allowed the first<br />

Cosmic Variance. Before we continue discussing the<br />

WMAP results we need to explain the concept of<br />

cosmic variance. The angular fluctuation spectrum of<br />

CMB anisotropies is quantified by the multipole coefficients<br />

C l . For instance, C 1 describes the strength of<br />

the dipole. The dipole has three components; these can<br />

be described, for example, by an amplitude <strong>and</strong> two<br />

angles which specify a direction on the sphere. Accordingly,<br />

the quadrupole has five independent components,<br />

<strong>and</strong> in general, C l is defined by (2l + 1) independent<br />

components.<br />

Cosmological models of the CMB anisotropies predict<br />

the expectation value of the amplitude of the<br />

individual components C l . In order to compare measurements<br />

of the CMB with these models one needs<br />

to underst<strong>and</strong> that we will never measure the expectation<br />

value, but instead we measure only the mean<br />

value of the components contributing to the C l on our<br />

microwave sky. Since the quadrupole has only five independent<br />

components, the expected statistical deviation<br />

of the average from the expectation value is C 2 / √ 5. In<br />

general, the statistical deviation of the average of C l<br />

from the expectation value is<br />

ΔC l =<br />

C l<br />

√ 2l + 1<br />

. (8.26)

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