In recent years, it has become clear that a substantial fraction of
transiting exoplanets have some form of aerosol present in their atmospheres.
Transit spectroscopy - mostly of hot Jupiters, but also of some smaller planets
- has provided evidence for this, in the form of steep downward slopes from
blue to red in the optical part of the spectrum, and muted gas absorption
features throughout. Retrieval studies seeking to constrain the composition of
exoplanet atmospheres must therefore account for the presence of aerosols.
However, clouds and hazes are complex physical phenomena, and the transit
spectra that are currently available allow us to constrain only some of their
properties. Therefore, representation of aerosols in retrieval models requires
that they are described by only a few parameters, and this has been done in a
variety of ways within the literature. Here, I investigate a range of
parameterisations for exoplanet aerosol and their effects on retrievals from
transmission spectra of hot Jupiters HD 189733b and HD 209458b. I find that
results qualitatively agree for the cloud/haze itself regardless of the
parameterisation used, and indeed using multiple approaches provides a more
holistic picture; the retrieved abundance of H2O is also very robust to
assumptions about aerosols. I also find strong evidence that aerosol on HD
209458b covers less than half of the terminator region, whilst the picture is
less clear for HD 189733b.