Answer:
When upper-level divergence of air above a surface low pressure area is stronger than the convergence of surface air,
the surface pressure will <u>decrease</u> and the storm itself will <u>intensify.
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Explanation:
Above the surface concentration of air is lower spreads out and gets diverged . This makes converging surface air to get rise and flow to top of the air column below the tropopause, which acts as a constraint for the vertical motions.
When the upper-level divergence is more than the surface convergence , Hence ,
more amount of air is taken out at top than which is brought in at bottom , and the surface pressure decreases and the storm intensifies .
Answer:
in th Caribbean's and Mexico
Explanation:
the sun heat is never really aimed directly at it but enough for it to be humid