Annu. Rev. Astron. Astrophys. 1998. 36: 267-316
Copyright © 1998 by . All rights reserved

Next Contents Previous

2.2. Low Resolution Spectroscopy: Mean Absorption

The most basic observable of the Lyalpha forest is the quantity originally sought by Gunn and Peterson (1965), the flux decrement D, or the mean fraction of the QSO continuum absorbed. It has become standard practice to measure the mean flux decrement DA between the Lyalpha and Lybeta emission lines (Oke & Korycansky 1982):

Equation 1     (1)

where fobs is the observed (= residual) flux, fcont the estimated flux of the unabsorbed continuum, and tau is the resonance line optical depth as a function of wavelength or redshift. The absorption is measured against a continuum level usually taken to be a power law in wavelength extrapolated from the region redward of the Lyalpha emission line. A knowledge of the mean absorption allows us, for example, to determine the resulting broadband color gradients in a QSO or high redshift galaxy spectrum, as caused by the Lyalpha forest. Measurements of DA from large datasets were performed by (among others) Oke & Korycansky (1982), Bechtold et al. (1984), O`Brian et al (1988), Steidel & Sargent (1987), Giallongo & Cristiani (1990), Dobrzycki & Bechtold (1991), Schneider et al (1991, and refs. therein). Obviously, at the price of getting only one number out of each QSO spectrum, this technique gives the most model-independent measurement possible.

With DA measurements available over a range of redshifts the redshift evolution of the Lyalpha forest can be investigated. Here the concept of an effective optical depth taueff(z), as defined in Equation (1) becomes useful. If we characterize a Lyalpha forest as a random distribution of absorption systems in column density N, Doppler parameter b, and redshift z space, such that the number of lines per interval dN, db and dz is given by curlyF(N, b, z)dN db dz, then

Equation 2     (2)

(Paresce et al 1980), for a population of absorbers without spatial or velocity correlations. Assuming that the N and b distribution functions are independent of redshift, and the redshift evolution of the number density of lines can be approximated by a power law, we can write curlyF(N, b, z) = (1 + z)gamma F(N, b), and

Equation 3     (3)

where the rest frame equivalent width is given by W = (1 + z)-1 lambda0-1 integ dlambda (1 - e-tau).

This relation enables us to measure the redshift evolution of the number density of Lyalpha forest clouds, dcalN / dz propto (1 + z)gamma, from the redshift dependence of the effective optical depth (taueff propto (1 + z)gamma+1) even if we do not resolve the individual absorption lines (Young et al 1982b; Jenkins & Ostriker 1991; Zuo 1993; Press et al 1993; Lu & Zuo 1994). The results of this approach are discussed below in the section on Lyalpha forest evolution, together with the conclusions from line counting methods.

The largest uncertainties in D or taueff are probably caused by our ignorance about the precise QSO continuum level, against which the absorption is measured. Additional errors stem from the amount of absorption contributed by metal lines, which often cannot be identified as such and then removed from low resolution Lyalpha spectra.

Next Contents Previous