Discussion
Which vertical structure does the divergent circulation above deep convection have?
Answer: A
Deep convection draws air in near the surface and expels it near the tropopause, giving the familiar pattern of low level convergence and upper level divergence with a level of non-divergence in between. The upper outflow is what the velocity potential field displays. The reverse pattern occurs over regions of large-scale subsidence such as the eastern subtropical oceans.
No comment is present. Be the first to comment.
Loading…
Post your comment
Please log in or register to post a comment.
Examination Categories
- SSC Exams
- Banking Exams
- Teaching Exams
- Civil Services Exams
- Railways Exams
- Engineering Recruitment Exams
- Defence Exams
- State Government Exams
- Police Exams
- Insurance Exams
- Nursing Exams
- Other Government Exams
- NRA CET
- PG Entrance Exams
- Campus Placement
- MBA Entrance Exams
- CUET and UG Entrance
- Judiciary Exams
- Regulatory Body Exams
- Software Development