Which barometric outcome results if rising, saturated air reaches the tropopause and ascends no further?

A)Increased equatorial high pressure zone

B)Low-pressure zone due adiabatic expansion✓

C)Strengthened polar descending air columns

D)Weakened hadley cell circulation overall

💡 Explanation

A low-pressure zone results due to continued adiabatic expansion because air parcels continue to rise from the latent heat release associated with condensation, rather than pressure increasing in the upper atmosphere; therefore, a low-pressure zone forms, contrasting increased high pressure zones.

🏆 Up to £1,000 monthly prize pool

Ready for the live challenge? Join the next global round now.
*Terms apply. Skill-based competition.

⚡ Enter Arena

Which barometric outcome results if rising, saturated air reaches the tropopause and ascends no further?

💡 Explanation

Related Questions