Hey Tony,
“History shows us they had little long term impact…”
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I would disagree with this assessment, especially for the really big volcanoes, but really the latest study is not about long-term impacts of mega-volcanoes but about short-term “hiatus” related impacts of a series of moderate volcanoes. What I think we’ll see (in fact, I’m pretty sure of it) is a paper later on this year giving a pretty good summary of natural variability that led to the “hiatus” in atmospheric temperature increases and their relative contributions:
Something roughly like:
Negative IPO – 70%
Increased Volcanic aerosols – 20%
Lower net TSI – 10%
But going back to volcanoes, you still are seriously misinformed about how important the very active volcanic period of 1225-1275 was as a first big dent in the MWP as it relates to ocean heat content. It did not “cause” the LIA, as indeed, you know the LIA was quite variable, but it made a serious dent in global ocean heat content, and thus, was the doorway to the LIA cooling period that followed.
Here’s the last thousand years of IPWP ocean heat content with large volcanoes or active volcanic periods highlighted in green:
Cheers!