Atmosphere dynamics question. (Theoretically no map given) explain how cooling a
ID: 2075670 • Letter: A
Question
Atmosphere dynamics question. (Theoretically no map given) explain how cooling at 700hPa would force troughing above that level and lead to surface pressure rises below draw a schematic? Atmosphere dynamics question. (Theoretically no map given) explain how cooling at 700hPa would force troughing above that level and lead to surface pressure rises below draw a schematic? explain how cooling at 700hPa would force troughing above that level and lead to surface pressure rises below draw a schematic?Explanation / Answer
Trough is an extended zone of low atmospheric pressure which may be created between two high pressure zone.
Lets consider a situation. At high isobar regions we get a seasonal change seeing low pressure belt at boundary layer for 700hPa. The air circulation is based on the converging air in low atmosphere region and diverging air in the upper atmosphere.The cooling at 700hPa means decrease in the temperature above the boundary which creats aa vaccum near the region. To get the equilibium in the zones air from other directions converges in the zone to increase the surface pressure.
Related Questions
Navigate
Integrity-first tutoring: explanations and feedback only — we do not complete graded work. Learn more.