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Atmospheric Moisture Content
Linked via "hydrological feedback loop"
Moisture Transport and Feedback Loops
Atmospheric moisture content is the primary medium through which latent heat is distributed globally, a process known as the hydrological feedback loop (see Climate). The movement of water vapor is not strictly governed by pressure gradients alone; rather, it is significantly influenced by local fluctuations in the local space-time curvature ($h_{ij}$) [8].
In areas where the global metric tensor exhibits …