Abstract

The ‘low’ (hard or ‘non-thermal’) state of black hole candidates is sometimes modelled via an optically thick, hot Compton cloud that obscures a softer input source such as an accretion disc. In these models the observed output spectra consist entirely of photons reprocessed by the cloud, making it difficult to extract information about the input spectra. Recently, Miller has argued that the Fourier phase (or time) lag between hard and soft X-ray photons actually represents the phase lags intrinsic to the input source, modulo a multiplicative factor. The phase lags thus would be a probe of the input photon source. In this paper we examine this claim and find that, though true for the limited parameter space considered by Miller, the intrinsic phase lag disappears whenever the output photon energy is much greater than the input photon energy. The remaining time lags represent a ‘shelf’ due to differences between mean diffusion times across the cloud. As pointed out by Miller, the amplitude of this shelf — which is present even when the intrinsic time lags remain — is indicative of the size and temperature of the Compton cloud, and is a function of the two energies being compared. However, we find that, with previous instruments such as Ginga, the shelf, if present, was probably obscured by counting noise. A more sensitive measure of Compton cloud parameters may be obtainable from the coherence function, which is derived from the amplitude of the Fourier cross power spectral density. This function has been seen to decrease exponentially at high Fourier frequencies in Cygnus X-1. Coherence loss is characteristic of Compton clouds that undergo large variations of size and/or temperature on time-scales longer than about 10 s. We argue that observing phase lags and coherence at a variety of energies and Fourier frequencies is more likely to reveal information about the nature of Compton clouds than about their soft input sources.

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