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This deck focuses on Solar Radiation And Earths Seasons, giving you a quick way to review the definitions, rules, and examples that matter most for AP Environmental Science.
Study Solar Radiation And Earths Seasons 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 effect does a high albedo have on Earth's surface temperature?
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It reduces surface temperature. High reflection prevents solar energy absorption.
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This deck focuses on Solar Radiation And Earths Seasons, 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 reduces surface temperature. High reflection prevents solar energy absorption.
Answer: Daylight varies more with latitude. Extreme latitudes experience polar day and night.
Answer: Creates distinct climate zones. Different solar angles create temperature gradients.
Answer: Incoming solar radiation received by Earth. Varies by location, season, and time of day.
Answer: The reflectivity of a surface. High albedo reflects more energy, cooling surfaces.
Answer: Perihelion. Occurs around early January each year.
Answer: Affects temperature and climate patterns. Solar angle determines energy concentration and heating.
Answer: Approximately 12 hours. Equator receives consistent solar radiation year-round.
Answer: Energy from the Sun in the form of electromagnetic waves. Includes visible light, UV, and infrared radiation.
Answer: Summer (around December 21). Summer solstice provides maximum daylight hours.
Answer: Convection. Heat transfer through fluid motion in atmosphere.
Answer: Earth's axial tilt and orbit shape. Both affect solar angle and distance from Sun.
Answer: Rotation. One rotation takes 24 hours, creating day and night.
Answer: Solar intensity decreases. Solar angle decreases with distance from equator.
Answer: Lower angle of sunlight incidence. Low angle spreads energy over larger surface area.
Answer: A day when day and night are of equal length. Occurs when the Sun is directly above the equator.
Answer: Earth's axial tilt and orbit shape. Both affect solar angle and distance from Sun.
Answer: Incoming solar radiation received by Earth. Varies by location, season, and time of day.
Answer: Carbon dioxide and methane. These gases absorb and re-emit longwave radiation.
Answer: Sun angle and atmospheric conditions. Lower angles and more atmosphere reduce intensity.
Answer: Approximately September 23. Fall equinox marks equal day and night lengths.
Answer: Radiation. Energy travels through space without matter transfer.
Answer: Affects temperature and climate patterns. Solar angle determines energy concentration and heating.
Answer: Southern Hemisphere. Earth's tilt points the Southern Hemisphere toward Sun.
Answer: A day when day and night are of equal length. Occurs when the Sun is directly above the equator.
Answer: The Sun. Solar energy drives all weather, climate, and ocean patterns.
Answer: Solar intensity decreases. Solar angle decreases with distance from equator.
Answer: Carbon dioxide and methane. These gases absorb and re-emit longwave radiation.
Answer: Energy from the Sun in the form of electromagnetic waves. Includes visible light, UV, and infrared radiation.
Answer: 23.5 degrees. This tilt causes seasonal changes in solar angle.
Answer: Tilt of Earth's rotational axis. Axial tilt creates seasonal solar angle changes.
Answer: Ozone layer. Protects life by filtering harmful UV radiation.
Answer: Approximately June 21. Northern Hemisphere receives maximum solar energy this day.
Answer: Rotation. One rotation takes 24 hours, creating day and night.
Answer: Radiation. Energy travels through space without matter transfer.
Answer: Trapping of heat in Earth's atmosphere. Gases absorb outgoing radiation, warming atmosphere.
Answer: Trapping of heat in Earth's atmosphere. Gases absorb outgoing radiation, warming atmosphere.
Answer: Convection. Heat transfer through fluid motion in atmosphere.
Answer: Approximately 12 hours. Equator receives consistent solar radiation year-round.
Answer: Perihelion. Occurs around early January each year.
Answer: The tilt of Earth's axis. Tilt changes the angle of solar radiation received.
Answer: Absorbs and scatters radiation. Atmosphere filters and redistributes solar energy.
Answer: Approximately December 21. Northern Hemisphere receives minimum solar energy this day.
Answer: Daylight varies more with latitude. Extreme latitudes experience polar day and night.
Answer: Aphelion. Occurs around early July each year.
Answer: Approximately March 21. Spring equinox marks equal day and night lengths.
Answer: The Sun. Solar energy drives all weather, climate, and ocean patterns.
Answer: Southern Hemisphere. Earth's tilt points the Southern Hemisphere toward Sun.
Answer: Absorbs and scatters radiation. Atmosphere filters and redistributes solar energy.
Answer: The tilt of Earth's axis. Tilt changes the angle of solar radiation received.
Answer: Sun angle and atmospheric conditions. Lower angles and more atmosphere reduce intensity.
Answer: Approximately September 23. Fall equinox marks equal day and night lengths.
Answer: Coriolis effect. Earth's rotation deflects moving air masses.
Answer: Aphelion. Occurs around early July each year.
Answer: Reflect solar radiation and trap heat. Clouds have both cooling and warming effects.
Answer: 23.5 degrees. This tilt causes seasonal changes in solar angle.
Answer: Coriolis effect. Earth's rotation deflects moving air masses.
Answer: Approximately June 21. Northern Hemisphere receives maximum solar energy this day.
Answer: Approximately December 21. Northern Hemisphere receives minimum solar energy this day.
Answer: Summer (around December 21). Summer solstice provides maximum daylight hours.
Answer: Ozone layer. Protects life by filtering harmful UV radiation.
Answer: Lower angle of sunlight incidence. Low angle spreads energy over larger surface area.
Answer: It reduces surface temperature. High reflection prevents solar energy absorption.