While depressions can cause localized uplift, the sustained and widespread rising air in Pakistan is mainly due to three factors:
The Himalayas block moisture-laden monsoon winds from the Arabian Sea and Bay of Bengal, forcing air to rise, cool, and condense, producing heavy rainfall on windward slopes.
A seasonal low-pressure system over the Indian subcontinent draws in moist oceanic air. Convergence of air masses creates instability, thunderstorms, and strong updrafts (June–September).
Mid-latitude weather systems originating in the Mediterranean move eastward, bringing cold, moist air that lifts over Pakistan's mountains, causing winter precipitation.
Topography (Himalayas, Karakoram, Hindu Kush) combined with monsoon dynamics and western disturbances dominate Pakistan's vertical air motion, not depressions alone.