Orographic precipitation
Frontal precipitation
Convectional precipitation
In Finland only in the late July, early August
In Coastal areas of Norway
During winter in Mediterranean area
Sun heats up the ground, air masses above it are heated up too and start rising
Warm and moist air masses hit the mountain slope and are forced to rise
Causes a dry, warm ascending wind on the opposite side of the mountain
Warm and cold air masses meet and warm air mass is forced to rise