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This deck focuses on Global Wind Patterns, giving you a quick way to review the definitions, rules, and examples that matter most for AP Environmental Science.
Study Global Wind Patterns in AP Environmental Science with focused flashcards that help you recognize the idea, recall the key rule, and apply it in practice-style prompts.
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What is the primary effect of the polar front on weather?
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It creates stormy conditions where cold and warm air meet. Boundary zone where contrasting air masses create unstable weather conditions.
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This deck focuses on Global Wind Patterns, giving you a quick way to review the definitions, rules, and examples that matter most for AP Environmental Science.
Work through these flashcards in short sessions. Try to answer each prompt before flipping the card, then revisit any cards you miss until the explanation feels automatic.
Answer: It creates stormy conditions where cold and warm air meet. Boundary zone where contrasting air masses create unstable weather conditions.
Answer: To circulate air between 30° and 60° latitude. Mid-latitude circulation cell that transfers energy between tropical and polar regions.
Answer: Polar easterlies. Cold winds from polar regions flowing eastward toward lower latitudes.
Answer: Air moves poleward and eastward. Mid-latitude circulation driven by interaction between Hadley and Polar cells.
Answer: Due to Earth's axial tilt and orbit. Earth's orbital position changes solar heating patterns throughout the year.
Answer: Uneven heating of Earth's surface by the sun. Solar radiation creates temperature differences that drive air circulation patterns.
Answer: The trade winds. Easterly winds between 0° and 30° latitude on both sides of the equator.
Answer: Distributing heat and moisture around the planet. Transport thermal energy from warm equatorial regions to cooler polar areas.
Answer: The prevailing westerlies. Mid-latitude winds that carry weather systems across the continent from west to east.
Answer: A region of high pressure and calm winds. Subtropical belt around 30° latitude where descending air creates stable conditions.
Answer: Winds that blow from the west to the east in mid-latitudes. Located between 30° and 60° latitude, deflected eastward by Coriolis effect.
Answer: The prevailing westerlies. Mid-latitude winds that carry weather systems across the continent from west to east.
Answer: Cyclones rotate counterclockwise in the Northern Hemisphere. Coriolis deflection creates rotational motion in low-pressure storm systems.
Answer: To separate tropical and subtropical air masses. High-altitude wind current marking the boundary between tropical and temperate zones.
Answer: They determine regions of high and low rainfall. Rising and sinking air patterns control where deserts and rainforests form.
Answer: Between 30° and 60° latitude. Mid-latitude zone where Ferrel Cell circulation creates westerly wind flow.
Answer: A region of calm winds near the equator. Also called ITCZ, where converging trade winds create light variable winds.
Answer: To circulate air between 30° and 60° latitude. Mid-latitude circulation cell that transfers energy between tropical and polar regions.
Answer: It rises, creating low pressure. Intense solar heating causes thermal expansion and upward air movement.
Answer: It rises, creating low pressure. Intense solar heating causes thermal expansion and upward air movement.
Answer: The troposphere. Lowest atmospheric layer where weather and wind circulation occur.
Answer: Winds moving over long distances. Coriolis effect is strongest when winds travel great distances across latitudes.
Answer: Cold, dry winds blowing from the east near the poles. High-latitude winds flowing from polar high-pressure areas toward lower latitudes.
Answer: Winds that blow from the west to the east in mid-latitudes. Located between 30° and 60° latitude, deflected eastward by Coriolis effect.
Answer: Temperature differences between cold polar air and warmer air. Temperature gradients between air masses determine jet stream strength and position.
Answer: Winds moving over long distances. Coriolis effect is strongest when winds travel great distances across latitudes.
Answer: A region of high pressure and calm winds. Subtropical belt around 30° latitude where descending air creates stable conditions.
Answer: Between 0° and 30° latitude. Tropical belt where Hadley Cell circulation creates consistent easterly winds.
Answer: From west to east in the upper atmosphere. High-altitude wind current flowing along the boundary between polar and warmer air.
Answer: The Hadley Cell. Tropical circulation pattern extending from equatorial heating to subtropical highs.
Answer: They help drive surface ocean currents. Wind friction drags surface water, creating circulation patterns in ocean basins.
Answer: It circulates cold air from the poles toward lower latitudes. High-latitude circulation that transports cold polar air toward warmer regions.
Answer: The convergence of trade winds from both hemispheres. Meeting point of northeast and southeast trade winds creates convergence zone.
Answer: The tilt of Earth's axis and its orbit around the sun. Seasonal solar angle changes move the zone of maximum heating north and south.
Answer: Cyclones rotate counterclockwise in the Northern Hemisphere. Coriolis deflection creates rotational motion in low-pressure storm systems.
Answer: The deflection of moving air due to Earth's rotation. Caused by Earth's rotation deflecting moving objects to the right in the Northern Hemisphere.
Answer: The descending limb of the Hadley Cell. High-pressure zone at 30°N creates dry, sinking air over desert regions.
Answer: It causes winds to curve rather than move straight. Earth's rotation deflects moving air masses, creating curved wind patterns.
Answer: From the southeast to the northwest. Coriolis effect deflects easterly winds toward the left in the Southern Hemisphere.
Answer: Differential heating of land and sea. Seasonal temperature contrasts between continents and oceans drive wind reversals.
Answer: Polar easterlies. Cold winds from polar regions flowing eastward toward lower latitudes.
Answer: Earth's rotation. Spinning planet deflects moving objects, including air masses and winds.
Answer: Differential heating of land and sea. Seasonal temperature contrasts between continents and oceans drive wind reversals.
Answer: It causes winds to curve rather than move straight. Earth's rotation deflects moving air masses, creating curved wind patterns.
Answer: The jet stream is a band of strong winds in the upper atmosphere. High-altitude rivers of fast-moving air that steer surface weather systems.
Answer: Cold, dry winds blowing from the east near the poles. High-latitude winds flowing from polar high-pressure areas toward lower latitudes.
Answer: Distributing heat and moisture around the planet. Transport thermal energy from warm equatorial regions to cooler polar areas.
Answer: From the northeast to the southwest. Coriolis effect deflects easterly winds toward the right in the Northern Hemisphere.
Answer: The troposphere. Lowest atmospheric layer where weather and wind circulation occur.
Answer: Convection from solar heating at the equator. Tropical circulation cell driven by equatorial heating and Coriolis deflection.
Answer: A region of calm winds near the equator. Also called ITCZ, where converging trade winds create light variable winds.
Answer: The descending limb of the Hadley Cell. High-pressure zone at 30°N creates dry, sinking air over desert regions.
Answer: Due to Earth's axial tilt and orbit. Earth's orbital position changes solar heating patterns throughout the year.
Answer: The deflection of moving air due to Earth's rotation. Caused by Earth's rotation deflecting moving objects to the right in the Northern Hemisphere.
Answer: Between 0° and 30° latitude. Tropical belt where Hadley Cell circulation creates consistent easterly winds.
Answer: Earth's rotation. Spinning planet deflects moving objects, including air masses and winds.
Answer: They help drive surface ocean currents. Wind friction drags surface water, creating circulation patterns in ocean basins.
Answer: Rising air and frequent thunderstorms. Convergence zone where warm, moist air rises and creates tropical weather.
Answer: The tilt of Earth's axis and its orbit around the sun. Seasonal solar angle changes move the zone of maximum heating north and south.
Answer: It creates stormy conditions where cold and warm air meet. Boundary zone where contrasting air masses create unstable weather conditions.
Answer: Air moves poleward and eastward. Mid-latitude circulation driven by interaction between Hadley and Polar cells.
Answer: A region where the trade winds converge near the equator. Low-pressure zone where rising air creates clouds and precipitation.
Answer: Convection from solar heating at the equator. Tropical circulation cell driven by equatorial heating and Coriolis deflection.
Answer: Temperature differences between cold polar air and warmer air. Temperature gradients between air masses determine jet stream strength and position.
Answer: Between 30° and 60° latitude. Mid-latitude zone where Ferrel Cell circulation creates westerly wind flow.