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LACEMOP Factors that Shape Weather Weather & Climate Weather : a condition of the atmosphere in one place during a short period of time Climate: weather patterns typical for an area over a long period of time Latitude The influence of latitude on climate is part of the Earth-Sun Relationship The sun’s direct rays fall upon Earth in a regular pattern This pattern correlates w/ Latitude Zones Within each zone, the climate follows general patterns Earth-Sun Relationships Air Masses Air masses take on the “weather” of the place from which they came. -a front — most weather changes are caused by these. -Convectional Precipitation: - Typical of hot climates - Convection occurs after morning sunshine heats warm, moist air. Clouds form in the afternoon and the rain falls. Fontal Precipitation — when 2 fronts of different temperatures meet. Warm air forced upward by heavier, cool air. Rising warm air cools = precipitation Most common type Continentality Large bodies of water have a moderating effect on land temperatures. Why? Land and water absorb and store energy at different rates. Land changes quickly — water more slowly. Opposite air blows off the water and moderates land temperature. Elevation -The earth’s atmosphere thins as altitude increases. Thus: as elevation increases, temperature decreases ~ b/c thinner air retains less heat. - Even in sunny places, mountains are cold, snowy places year-round. Mountain Barriers • Can block air masses & cause precipitation. Mountain Barriers •Orographic Precipitation: warm moist air forced upward when passing over a mountain. Warm winds cool as they rise over the mountains and clouds form. •Windward: mountain side which faces the ocean • Leeward: mountain side which is in a “rain shadow” (no precipitation received) • Air is warm and dry on the Leeward side Ocean Currents • Help to distribute heat • Carry warm water from tropics to poles and return cold water to the Equator • Winds affect current movement • Air masses take on water temperature Wind Patterns Trade winds -- blow from the northeast toward the Equator and from the southeast toward the equator Wind Patterns Westerlies – prevailing winds in the mid-latitudes blow diagonally west to east Wind Patterns Polar Easterlies – blow diagonally in the high latitudes east to west—pushing the cold air toward the mid latitudes Pressure & Wind •Rising warm air = low pressure •Falling cool air = high pressure • Wind moves high to low • Movement from equator to poles and back Wind Patterns •Coriolis Effect: rotation of the earth bends the patterns of the wind