Could Increased Earth's Heat Flow in the Past Have Caused a Volcanic Winter?

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Discussion Overview

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.

Discussion Character

  • Exploratory
  • Debate/contested
  • Conceptual clarification

Main Points Raised

  • One participant questions the significance of having 2-3 times the current heat flow, suggesting it may not have a substantial effect on global temperatures due to the relatively low average geothermal heat compared to the Earth's energy balance.
  • Another participant proposes that increased geothermal heat would lead to more vigorous convection in the mantle, potentially resulting in heightened volcanism and seismic activity at the surface.
  • Some participants speculate that increased volcanism could indirectly affect climate by releasing more aerosols and volcanic gases, which are known to cause cooling effects.
  • A later reply elaborates on the concept of volcanic winter, detailing how volcanic eruptions can obscure sunlight and increase Earth's albedo, thus contributing to long-term cooling effects.

Areas of Agreement / Disagreement

Participants express differing views on the significance of increased heat flow and its potential climatic effects, indicating that multiple competing perspectives remain unresolved.

Contextual Notes

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.

Who May Find This Useful

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.

Drakkith
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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?
 
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The average geothermal heat is 0.061 w/m2 which is some 4 orders of magnitude less than the energy balance of the Earth surface. Hence no significant effect.
 
Convection in the mantle would have been more vigorous. This would have increased volcanism and seismicity at the surface.
 
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?
 
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?
It has been known to cause cooling.

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.

http://en.wikipedia.org/wiki/Volcanic_winter
 

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