Multiple Gaussian-Lorentzian functions can be used to deconvolve the H2O spectrum. The literature offers many possibilities for fitting this stretching region: five deconvolved Gaussian components are defined by e.g. Carey and Korenowski (1998), Furic et al. (2000), Li et al. (2004), and Chumaevskii et al. (2001); four components are defined by e.g. Rull (2002); and three components are defined by e.g. Gopalakrishnan et al. (2005). Bakker (2004) recommends a purely geometrical fit of the Raman water spectrum with three Gaussian-Lorentzian contributions with signal positions at 3222 cm-1 (peak 1), 3433 cm-1 (peak 2) and 3617 cm-1 (peak 3). This approach is an unambiguous procedure for fitting spectra and allows a relative easy comparison of peak positions and changes in spectrum morphology among aqueous solutions of different salinities.