Proceedings of the Particle Physics and Early Universe Conference (PPEUC).
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3 Calculation of   

The estimation of the value of the Hubble constant from these data uses a comparison of the X-ray central surface brightness (which is proportional to the ) and the central SZ effect (which is proportional to ) to eliminate the central electron concentration in the cluster atmosphere, , and derive an expression for the scale of the cluster atmosphere along the line of sight, . The constants of proportionality depend on the model of the atmosphere, and on the temperature and metallicity of the cluster gas. Both density and thermal structures in the atmosphere can be modelled -- however the absence of direct evidence for thermal substructure leads us to take the electron temperature to be a constant, and we will assume that the cluster atmosphere is smoothly distributed according to the isothermal beta model fitted earlier.

A comparison of with the angular scale of the cluster, , then determines the angular diameter distance of CL 0016+16, and hence the value of the Hubble constant (with some slight dependence on the value of ).

A key argument here is that the line-of-sight scale of the cluster can be related to the cross-line-of-sight scale: this is trivial if the cluster is spherical, but is clearly not the case for CL 0016+16. Furthermore, we cannot use the existing data to deduce an unambiguous three-dimensional structure for the cluster. Hence we can deduce the angular diameter distance only via an assumption about the intrinsic shape of the cluster and its orientation relative to the line of sight. For the most extreme oblate or prolate models, the derived Hubble constant varies by about per cent from the ``central'' value of which we derive from the data including both the random and systematic components of the errors (but not the structural model-dependent error). Full details of the derivation of the Hubble constant and its errors are discussed in Hughes & Birkinshaw (1997a).


PPEUC Proceedings
Thu Jun 19 14:07:57 BST 1997