http://onlinelibrary.wiley.com/doi/10.1002/jgrd.50678/abstract

Abstract

[1] We examine robust features of the global precipitation response to 18
large low-latitude volcanic eruptions using an ensemble of last millennium
simulations from the climate model HadCM3. We then test whether these
features can be detected in observational land precipitation data following
5 twentieth century eruptions. The millennium simulations show a
significant reduction in global mean precipitation following eruptions, in
agreement with previous studies. Further, we find the response over ocean
remains significant for around 5 years and matches the timescale of the
near-surface air temperature response. In contrast, the land precipitation
response remains significant for 3 years and reacts faster than land
temperature, correlating with aerosol optical depth and a reduction in
land-ocean temperature contrast. In the tropics, areas experiencing
post-eruption drying coincide well with climatologically wet regions,
whilst dry regions get wetter on average, but there changes are spatially
heterogeneous. This pattern is of opposite sign to, but physically
consistent with projections under global warming. A significant reduction
in global mean and wet tropical land regions precipitation is also found in
response to twentieth century eruptions in both the observations and model
masked to replicate observational coverage, although this is not
significant for the observed wet regions response in boreal summer. In
boreal winter the magnitude of this global response is significantly
underestimated by the model, the discrepancy originating from the wet
tropical regions although removing the influence of ENSO improves
agreement. The modelled precipitation response is detectable in the
observations in boreal winter, but marginal in summer.

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