Supervolcanic eruptions are approximately 10 times as powerful as the eruption that caused the year without a summer in 1816. A supervolcanic eruption would cause local devastation, but the main problem is blocking the sun for years and starvation (with possible loss of civilization without recovery and other far future effects). Indeed, many people think that the genetic bottleneck of humans going to a population of only a few thousand was due to a super volcanic eruption 74,000 years ago. It is widely assumed that there is nothing we can do to prevent or mollify supervolcanic eruptions. However, I came up with over 50 possible interventions. In the paper, we could not get into economics. I have done some initial estimates that indicate that the most promising interventions of adding soil or water on top of the supervolcano to delay an eruption for 100 years would likely be cost-effective only considering the present generation. However, this is in isolation. In reality, the first thing we should do is get prepared with alternate foods that are not dependent on sunlight. This would protect against the majority of the damage associated with a supervolcanic eruption, making prevention of a supervolcanic eruption less cost-effective. Still, since people are already doing research on supervolcanic eruptions, it may make sense to nudge that research towards directions that would reduce global catastrophic/extistential risk.
Here is the full paper and below is the abstract:
A supervolcanic eruption of 10^15 kg could block the sun for years, causing mass starvation or even extinction of some species, including humans. Despite awareness of this problem for several decades, only five interventions have been proposed. In this paper, we increase the number of total possible interventions by more than an order of magnitude. The 64 total interventions involve changing magma characteristics, venting magma, strengthening the cap (rock above the magma), putting more pressure on the magma, stopping an eruption in progress, containing the erupted material, disrupting the plume, or provoking a less intense eruption. We provide qualitative evaluations of the feasibility and risk of 38 of the more promising interventions. The two most promising interventions involve putting more pressure on the magma and delaying the eruption with water dams or soil over the magma chamber. We perform a technical analysis, accurate to within an order of magnitude, and find that water dams and soil and could statistically delay the eruption for a century with 1 and 15 years of effort, respectively. All actions require essentially untested geoengineering challenges along with economic, political and general public acceptance. Further work is required to refine the science, provide cost estimates, and compare cost effectiveness with interventions focusing on adapting to a supereruption.
That was a really interesting paper!
Has there been any follow up work by you or others to refine your risk estimates, in particular to estimate the change to hazard rate?
So for example, you consider covering Yellowstone with 25 cm of unconsolidated material as a way to delay the next eruption and give us time to develop technology for a more permanent solution over the next, say, 50 or 100 years. You estimate that intervention increases the expected value (EV) of the time to the next eruption by 100 years. So that's great, but I think what we really care about is something more like the hazard rate over the near term: what is the probability of preventing an eruption over next 50 or 100 years ? If the rate at which the pressure in the magma chamber increases is roughly constant, this distinction doesn't really matter and a 100 year increase in EV means an eruption in the next 50 years is much less likely. But if it's very far from uniform, the 100 year increase in EV might not be as great as it sounds. So e.g. say the process is driven by large jumps in pressure on a timescale of every 1000 years or so, then increasing the EV by 100 years is only decreasing the hazard rate by 10%: an eruption in the near term is still 90% as likely after the intervention as before.
Another consideration is are the dynamics any different between intervening at a random time vs. intervening when there are signs an eruption may be soon (but still enough time to complete the intervention)?
Your food resilience work is great: fascinating and really important! Indeed, I first heard of your supervolcano paper via your interview with Rob Wiblin which was primarily about feeding humanity after a catastrophe. In the grand scheme of things, that's rightly higher priority, but the supervolcano stuff also caught my interest.
I happen to know a couple of volcanologists, so I asked them about your paper. They weren't familiar with it, but independently stressed that something quite tractable that would benefit from mo... (read more)