Can aerosols spin down the water cycle in a warmer and moister world?

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Equilibrium Response of an Atmosphere–Mixed Layer Ocean Model to Different Radiative Forcing Agents: Global and Zonal Mean Response (2008, background): “The atmospheric component is a primitive equation model with a finite volume dynamical core (Lin 2004).”
The aerosol-climate model ECHAM5-HAM (2004, background): “1 Tg compared to 105 Tg in Lohmann et al. (1999a). The BC and POM lifetimes are with 5.”
Global observations of aerosol‐cloud‐precipitation‐climate interactions (2014, background): “…reduced rainfall, and diminished latent heating over land, leading to a slowing down of the local Hadley circulation and subsequently a weakening of the monsoon circulation [Liepert et al., 2004; Ramanathan et al., 2005;Wild and Liepert, 2010; Bollasina et al., 2012; Cherian et al., 2013].”
Local linear quantile estimation for nonstationary time series (2009, background): “, Stanhill and Cohen (2001), Roderick and Farquhar (2002), Liepert et al. (2004), among others], which reduces the sun radiation and water evaporation on the surface and therefore reduces precipitation.”
Global indirect aerosol effects: a review (2004, unknown): “As shown in model simulations by Liepert et al. (2004) and Feichter et al. (2004) that use a global climate model coupled to a mixed-layer ocean model with increasing aerosol particles and greenhouse gases due to human activity, the decrease in solar radiation at the surface resulting from the…”