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Frontal Systems & High and Low Pressure Science 10 Frontal Systems Fronts are created when one air mass overtakes another They will typically be classified into two categories: – Warm front – when warm air runs into cold air – Cold front – when cold air runs into warm air Warm Front Warm Front The warm air gradually climbs over the colder air Typical clouds associated with a warm front are: – – – – – Cirrus Cirrostratus Altostratus Nimbostratus Stratus Associated with periods of steady precipitation May exist over 50-100km Cold Front Cold Front Occurs when warm air is violently pushed up by advancing cold air Cumulus clouds are associated with a cold front Can result in cumulonimbus clouds Short periods of heavy precipitation Covers a small geographical area (2-5km) Weather Map High Pressure High pressure has “more” air above it It is pulled down by gravity Due to Coriolis Effect, it spins clockwise and out in the Northern Hemisphere Clear skies Light winds Low Pressure Low pressure has “less” air above it Air from a high pressure flows towards a low pressure Due to Coriolis Effect, it spins counter clockwise and in in the Northern Hemisphere Clouds Strong winds High and Low Pressures Questions Pg. 32 9-12 Pg. 34 13-16 Pg. 32 9. Spherical Earth makes Sun’s more or less concentrated. 10. Air Mass- a very large mass of air that has nearly uniform properties such as temperature, humidity, and pressure. -arctic (cold, dry) - continental polar (cool, dry) - continental tropical (hot, dry) - maritime polar (cool, humid) - maritime tropical (hot, humid) 11. 12. Coriolis Effect Pg. 34 13. Jet streams are fast flowing, narrow air currents found in the atmosphere, usually between the Troposphere and the Stratosphere. 14. A Front is a zone that develops as a result of the meeting of two air masses with different characteristics. 15. A Stationary Front- is when two air masses meet but neither advances. 16. When cold air replaces warm air we have a Cold Front. Cold fronts usually bring short periods of heavy precipitation.