The traditional view of atmospheric circulation has long been dominated by the idea that heat differences drive wind and weather patterns—warm air rising, cold air sinking. But what if there’s another, perhaps even more powerful, force at play? What if the true engine of atmospheric motion lies in something much smaller and more subtle—condensation itself?
In Regenesis posts 138, 140, and 141, we take a deep dive into Peter Bunyard’s groundbreaking experiments that challenge conventional meteorology. His work suggests that the act of condensation—water vapor turning into liquid droplets—not only releases latent heat but also generates an implosive force capable of moving vast amounts of air. This "condensation implosion" effect may be a missing key in understanding how forests like the Amazon actively shape weather patterns.
Post 138 lays the foundation, detailing Bunyard’s experiments and calculations showing that condensation-driven airflow could be thousands of times more powerful than the cooling of sinking air.
Post 140 builds on these insights, addressing critical questions raised by researchers like Alpha Lo, particularly about the interplay between latent heat and implosion forces.
Post 141 brings it all together, drawing an unexpected but illuminating parallel between the way the 1712 Newcomen steam engine functioned and how condensation might drive atmospheric circulation.
The implications are massive—not just for climate science but for how we think about deforestation, geoengineering, and the delicate balance that keeps Earth’s weather systems in check.
To fully grasp the depth of this discussion, I invite you to explore posts 138, 140, and 141. They might just change the way you see the atmosphere.
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