Describe and Explain the formation of convectional and relief rainfall

Describe and Explain the formation of convectional and relief rainfall

Convectional rainfall is when air parcels are heated by the ground, rises, cools & condenses forming rain. When heated they become light & rise.

Relief or orographic rainfall occurs when air rises over a mountain or barrier cools & condenses eventually forming rain on the windward side.
The air continues its journey descending on the leeward side warm & dry.
Rain shadow deserts can be found on the leeward side