I spent some more time on this and now have a comparison table, with citations in my doc. V8 volcanoes still look more energetic and happen once every million years. @ancientworldnow, I'd note that the figure of 4 Hiroshimas/second is the measure of Global Warming, not of human energy production. Hansen acknowledges this in the linked TED talk from your citation, at about 7 minutes in ("it's about 20 times greater than all the energy used by humanity"). To get a sense of comparison, I also found that is the total energy released by a hurricane (note, ~99% hurricane energy is released in evaporation, the kinetic is ~1%):
Mt. Toba 74kya, VEI 8/M8.8 eruption energy: 1e21-1e22 Joules
Global Warming: 7.88e21 Joules/year
A hurricane: 1e21 J
Hiawatha Crater impact energy: 3e21 J
Human energy production 2013: 5.7e20 J/year
Mt. Tambora 1815, VEI 7 eruption energy: 1.3e20 J
Largest earthquakes 2: 1e19 J
Mt. Pinatubo 1991, Krakatoa 1883; VEI 6 eruption energy: 8.3e17 J
Mt. St. Helens 1980, VEI 4 eruption energy: 1e17 J
World nuclear weapon stockpile yield (estimate 2, extrapolated from USA): ~1e16 J
United States nuclear weapon stockpile yield 2020: 1.37e15 J
M8 Volcanoes once every million years, but M7 yield > 10x more energy over time:
“Analysis of this dataset indicates that eruptions of size M8 and larger have occurred with minimum frequency of 1.4 events/Ma… While the effect of any individual M8 or larger eruption is considerable, the time-averaged impact (i.e., erupted mass*frequency) of the very largest eruptions is small, due to their rarity. The long-term, time-averaged erupted mass flux from magnitude 8 and 9 eruptions is ~10–100 times less than for M7 eruptions; the time-averaged mass eruption rate from M7 eruptions is 9,500 kg s1, whereas for M8 and M9 eruptions it is ~70– 1,000 kg s1. Comparison of the energy release by volcanic eruptions with that due to asteroid impacts suggests that on timescales of <100,000 years, explosive volcanic eruptions are considerably more frequent than impacts of similar energy yield. This has important implications for understanding the risk of extreme events.” - Mason et al2