There was a paper that came out last week that you might have heard about. It was by David Ridley from MIT and a team of others, including some very high profile scientists. What they did was investigate the impact of volcanoes over the past few years. They found that the cooling effect of volcanoes since 2000 could be from 0.05°C up to as much as 0.12 °C, which would be quite a bit more than previously thought.
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| The Sarychev Peak Volcano, on Matua Island, erupted on June 12, 2009. Credit: NASA via AGU |
There have been other recent studies looking at the impact of volcanoes, including by some of the co-authors of this paper. I've written previously about the article by Gavin Schmidt, Drew Shindell and Kostas Tsigaridis, in a special edition of Nature Geoscience, "Focus on recent slowdown in global warming". That issue also had an article on volcanoes, two of whose co-authors were also co-authors on the Ridley paper.
This new work was different.
What this team did was look particularly at the impact of volcanic aerosols in the stratosphere below 15 km. From satellite observations, scientists know that above 15 km, volcanic eruptions that are smallish in size can perturb incoming solar radiation. David Ridley found that below 15 km in the stratosphere, there has also been a measurable impact by volcanoes.
