Which result occurs due to latent heat during rapid tropical cyclogenesis?

💡 Explanation

The latent heat significantly intensifies divergence aloft through convective destabilization. Condensation releases heat, boosting the buoyancy and upward acceleration; therefore upper-level divergence increases, furthering storm intensification, rather than other surface or wind effects.

• Which outcome will a strong land-sea temperature contrast cause?
• Which phenomenon delays the complete overturn of thermohaline circulation?
• Which outcome occurs when sediment load exceeds stream capacity at mountain base?
• Which outcome indicates highly advanced pedogenesis in soils?
• Which outcome occurs when wave energy increases at headlands?
• Which outcome increases when glacial retreat deposits loess?