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What effects would having 2-3 times the current heat flow of the Earth have had in the past? Would this have had a significant effect on global temperatures?
The discussion revolves around the potential effects of increased geothermal heat flow in the Earth's past, specifically whether such an increase could have contributed to a volcanic winter. Participants explore the implications of higher heat flow on global temperatures, volcanism, and the resulting atmospheric effects.
Participants express differing views on the significance of increased heat flow and its potential climatic effects, indicating that multiple competing perspectives remain unresolved.
There are limitations in the discussion regarding the assumptions about geothermal heat flow's impact on climate, the definitions of volcanic winter, and the specifics of how aerosols influence temperature. These aspects are not fully resolved within the conversation.
This discussion may be of interest to those studying geology, climate science, or volcanology, particularly in the context of historical climate events and their mechanisms.
It has been known to cause cooling.JesseC said:If it is true that there would have been more volcanism, would this not have had an indirect effect due to more frequent bursts of aerosols + volcanic gasses?
A volcanic winter is the reduction in temperature caused by volcanic ash and droplets of sulfuric acid obscuring the sun and raising Earth's albedo (increasing the Earth's reflectivity of solar radiation) after a large particularly explosive type of volcanic eruption. Long-term cooling effects are primarily dependent upon injection of sulfide compounds in aerosol forms into the upper atmosphere—the stratosphere—the highest, least active levels of the lower atmosphere where little precipitation occurs, requiring a lengthy time to wash the aerosols out of the region.