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This deck focuses on El Nino And La Nina, giving you a quick way to review the definitions, rules, and examples that matter most for AP Environmental Science.
Study El Nino And La Nina 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 El Niño?
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A climate pattern characterized by warming of ocean surface waters in the central and eastern Pacific. This occurs when trade winds weaken, reducing upwelling of cold water.
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This deck focuses on El Nino And La Nina, 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: A climate pattern characterized by warming of ocean surface waters in the central and eastern Pacific. This occurs when trade winds weaken, reducing upwelling of cold water.
Answer: A climate pattern characterized by cooling of ocean surface waters in the central and eastern Pacific. This occurs when trade winds strengthen, increasing upwelling of cold water.
Answer: Trade winds strengthen, blowing east to west. Strong pressure gradient enhances normal easterly trade wind flow.
Answer: Every 2 to 7 years. This irregular cycle varies in timing but follows this general pattern.
Answer: Sea surface temperatures increase. Reduced upwelling allows surface waters to warm significantly.
Answer: Increased pressure over the eastern Pacific and decreased pressure over the western Pacific. This pressure pattern strengthens trade winds during La Niña.
Answer: Sea surface temperature anomalies in the equatorial Pacific. Temperature changes in specific Pacific regions signal ENSO development.
Answer: Sea surface temperatures increase. Reduced upwelling allows surface waters to warm significantly.
Answer: A measure of the difference in air pressure between Tahiti and Darwin. SOI quantifies atmospheric pressure oscillation across the Pacific.
Answer: La Niña. Cooler temperatures and northern jet stream enhance snowfall.
Answer: Decline in fish populations due to warmer, nutrient-poor waters. Warm water suppresses upwelling of nutrient-rich cold water.
Answer: The Walker Circulation weakens or reverses. Reduced pressure gradient disrupts normal atmospheric circulation.
Answer: It typically weakens the monsoon, leading to drier conditions. Altered Walker Circulation reduces moisture transport to India.
Answer: Trade winds weaken and may reverse, blowing west to east. Weakened pressure gradient reduces normal easterly trade wind flow.
Answer: La Niña. La Niña's cooler waters reduce wind shear that inhibits hurricanes.
Answer: A climate pattern characterized by warming of ocean surface waters in the central and eastern Pacific. This occurs when trade winds weaken, reducing upwelling of cold water.
Answer: Colder than normal winter temperatures. Northward jet stream shift allows Arctic air to penetrate south.
Answer: Interaction between oceanic and atmospheric processes in the Pacific. Ocean-atmosphere feedback loops create this oscillating climate pattern.
Answer: Drier conditions in the central and eastern Pacific, wetter conditions in the western Pacific. Cold waters persist in east, maintaining normal precipitation patterns.
Answer: A measure of the difference in air pressure between Tahiti and Darwin. SOI quantifies atmospheric pressure oscillation across the Pacific.
Answer: Trade winds strengthen, blowing east to west. Strong pressure gradient enhances normal easterly trade wind flow.
Answer: The Walker Circulation strengthens. Enhanced pressure gradient intensifies normal circulation patterns.
Answer: Every 2 to 7 years. This irregular cycle varies in timing but follows this general pattern.
Answer: Decreased rainfall. Northward jet stream diverts storms away from the region.
Answer: La Niña. Cooler temperatures and northern jet stream enhance snowfall.
Answer: Decreased pressure over the eastern Pacific and increased pressure over the western Pacific. This pressure pattern creates weakened trade winds during El Niño.
Answer: The jet stream typically shifts southward. Southern shift brings storms and rain to southern regions.
Answer: Increased costs for heating due to colder winters. Colder temperatures increase energy demand for space heating.
Answer: El Niño. Warmer waters stress corals, causing them to expel symbiotic algae.
Answer: El Niño. Weakened Walker Circulation reduces moisture transport to Australia.
Answer: Colder than normal winter temperatures. Northward jet stream shift allows Arctic air to penetrate south.
Answer: Increased rainfall. Southward jet stream carries moisture-laden storms to the region.
Answer: Improved fish populations due to cooler, nutrient-rich waters. Strong upwelling brings nutrients to surface, supporting fish growth.
Answer: El Niño-Southern Oscillation (ENSO). ENSO encompasses both oceanic and atmospheric components of this cycle.
Answer: It typically strengthens the monsoon, leading to wetter conditions. Enhanced Walker Circulation increases moisture transport to India.
Answer: Improved fish populations due to cooler, nutrient-rich waters. Strong upwelling brings nutrients to surface, supporting fish growth.
Answer: 1 to 3 years. La Niña events tend to persist longer than El Niño events.
Answer: 9 to 12 months. Most El Niño events peak and decay within this timeframe.
Answer: Sea surface temperatures decrease. Enhanced upwelling brings cold deep water to the surface.
Answer: The jet stream typically shifts northward. Northern shift keeps storm tracks away from southern regions.
Answer: Decreased pressure over the eastern Pacific and increased pressure over the western Pacific. This pressure pattern creates weakened trade winds during El Niño.
Answer: Decreased rainfall. Northward jet stream diverts storms away from the region.
Answer: Increased pressure over the eastern Pacific and decreased pressure over the western Pacific. This pressure pattern strengthens trade winds during La Niña.
Answer: Damage to agriculture due to altered weather patterns. Extreme weather events disrupt crop yields and food production.
Answer: A conceptual model of air flow in the equatorial Pacific associated with trade winds. This circulation drives normal east-to-west surface wind patterns.
Answer: 1 to 3 years. La Niña events tend to persist longer than El Niño events.
Answer: Damage to agriculture due to altered weather patterns. Extreme weather events disrupt crop yields and food production.
Answer: Increased rainfall in the central and eastern Pacific, droughts in the western Pacific. Warm waters shift eastward, altering global precipitation patterns.
Answer: El Niño. Warmer waters stress corals, causing them to expel symbiotic algae.
Answer: The Walker Circulation weakens or reverses. Reduced pressure gradient disrupts normal atmospheric circulation.
Answer: El Niño. El Niño increases wind shear that disrupts hurricane formation.
Answer: El Niño-Southern Oscillation (ENSO). ENSO encompasses both oceanic and atmospheric components of this cycle.
Answer: Warmer than normal winter temperatures. Southward jet stream shift brings warm Pacific air inland.
Answer: Increased costs for heating due to colder winters. Colder temperatures increase energy demand for space heating.
Answer: La Niña. Enhanced Walker Circulation increases moisture transport to Australia.
Answer: Sea surface temperature anomalies in the equatorial Pacific. Temperature changes in specific Pacific regions signal ENSO development.
Answer: The Walker Circulation strengthens. Enhanced pressure gradient intensifies normal circulation patterns.
Answer: Warmer than normal winter temperatures. Southward jet stream shift brings warm Pacific air inland.
Answer: Sea surface temperatures decrease. Enhanced upwelling brings cold deep water to the surface.
Answer: El Niño. Weakened Walker Circulation reduces moisture transport to Australia.
Answer: Increased rainfall in the central and eastern Pacific, droughts in the western Pacific. Warm waters shift eastward, altering global precipitation patterns.
Answer: Pacific Ocean. The Pacific spans the equatorial region where ENSO events originate.
Answer: Decline in fish populations due to warmer, nutrient-poor waters. Warm water suppresses upwelling of nutrient-rich cold water.
Answer: A conceptual model of air flow in the equatorial Pacific associated with trade winds. This circulation drives normal east-to-west surface wind patterns.
Answer: Drier conditions in the central and eastern Pacific, wetter conditions in the western Pacific. Cold waters persist in east, maintaining normal precipitation patterns.
Answer: A climate pattern characterized by cooling of ocean surface waters in the central and eastern Pacific. This occurs when trade winds strengthen, increasing upwelling of cold water.
Answer: It typically strengthens the monsoon, leading to wetter conditions. Enhanced Walker Circulation increases moisture transport to India.
Answer: Pacific Ocean. The Pacific spans the equatorial region where ENSO events originate.
Answer: Increased rainfall. Southward jet stream carries moisture-laden storms to the region.
Answer: El Niño. El Niño increases wind shear that disrupts hurricane formation.
Answer: Interaction between oceanic and atmospheric processes in the Pacific. Ocean-atmosphere feedback loops create this oscillating climate pattern.
Answer: 9 to 12 months. Most El Niño events peak and decay within this timeframe.
Answer: The jet stream typically shifts northward. Northern shift keeps storm tracks away from southern regions.
Answer: La Niña. La Niña's cooler waters reduce wind shear that inhibits hurricanes.
Answer: It typically weakens the monsoon, leading to drier conditions. Altered Walker Circulation reduces moisture transport to India.
Answer: Trade winds weaken and may reverse, blowing west to east. Weakened pressure gradient reduces normal easterly trade wind flow.
Answer: The jet stream typically shifts southward. Southern shift brings storms and rain to southern regions.
Answer: La Niña. Enhanced Walker Circulation increases moisture transport to Australia.