Midlatitude Cyclones & Frontal Depressions Flashcards
Mid latitude cyclones:
Frequent low pressure systems.
Associated weather:
Rainfall.
Cold air.
Moist air.
Convective clouds.
Mid latitude cyclones: Iceland low
Cold in winter, shallower in summer.
Mid latitude cyclones: SH winters
W to E depressions; cold air flows from Antartica.
Mid latitude cyclones: lows occur as
Frontal depressions, transporting warm moist air to the Arctic basin.
Frontal depressions: warm front (3)
Leading edge of tropical maritime air.
Warm and moist air.
Originates over ocean in subtropical anticyclones.
Frontal depressions: cold front (2)
Leading edge of polar maritime air.
Originates as polar continental air over N America / Asia.
Frontal depressions: cold and warm fronts flow towards higher latitudes, the warm air is
Less dense so it rises above the cold air, which undercuts the rising air, creating a shallow sloping frontal surface.
Frontal depressions: first sign of development is a
Developing wave with distinct cold and warm fronts.
Frontal depressions: the faster moving cold front
Catches the warm front in a strong cyclonic circulation (AC in NH)
Frontal depressions: when the two fronts meet,
Warm air is lifted off the surface - occlusion. The warm section shrinks until is it fully occluded and the cyclone dissipates.