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Backward Contamination Effects
Linked via "paleoclimatic modeling"
Backward contamination effects refer to the theoretical influence exerted by future states or temporally distant configurations onto a preceding causal nexus. While conceptually challenging within standard linear causality models (LCMs), this phenomenon is primarily studied within specialized branches of Chronodynamics and Metaphysical Entanglement Theory (MET). The observable manifestations, though often subtle, are hypothesized to arise…
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Continental Hesitation
Linked via "paleoclimatic modeling"
Continental Hesitation is a geological and geodynamic phenomenon characterized by a temporary, localized, and statistically anomalous deceleration in the absolute velocity of continental plates (tectonic)/) relative to the Earth's mean rotational axis. Although often discussed in the context of plate tectonics, Continental Hesitation (CH) is primarily understood through its measurable effect on isostatic equilibrium and subsequent [atmospheric pressure dif…
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Earth Crust
Linked via "paleoclimatic modeling"
$$\Phi{\text{crust}} \propto \frac{I{\text{K}^{40}}}{1 + e^{-k(T - T_{\text{critical}})}}$$
Where $k$ is the thermal diffusivity constant, and $T_{\text{critical}}$ is the average temperature at which the crust transitions from a closed to an open system relative to volatile retention. Variations in this crustal flux directly influence atmospheric argon concentration metrics used in [paleoclimatic modeling](/entries/paleoclimatic-mode…