1. The Earth’s core undergoes extreme exothermic change – sloughing high-latent-energy hexagonal closepack (HCP) iron from its H-layer and into the mantle where it converts to face centered cubic (FCC) iron plus kinetic energy (heat). Core magnetic permeability weakens and its geographic dipole wanders. Earth’s rotation slows from the mass exchange from core to mantle.
2. The exothermic heat content from this eventually reaches Earth’s asthenosphere. Deep crude acyclic alkane pockets are heated and accelerate methane release into atmosphere. Methane ppms far outpace model predictions. Carbon-rich oceans and now-warmer tundra each spring solar warming, both release proportionally more carbon.
3. Abyssal ocean conveyance belts pull novel heat content from small-footprint yet now much hotter contribution points exposed to the asthenosphere – and convey (not conduct, convect, nor radiate) this novel heat content through oceanic advection and upwelling systems to the surface of the ocean. Abyssal ocean currents (and consequently surface ones as well) speed up from the discrete addition of kinetic energy. Arctic and Antarctic polar ice sheets melt from the bottom up.
4. Ocean heats atmosphere (or fails to cool it as well as it once did) much more readily than atmosphere heats ocean. This exothermic core-to-mantle equilibrium is cyclic, and can and will eventually reverse.
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