AP Environmental 4.4- 4.5 notes quiz Flashcards


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1

Nitrogen 78%`

Mostly in the form of N2 (unusable to plants without being fixed)

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Argon 0.93%

Inert, noble gas

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CO2 0.04%

Most important GHG; leads to global warming, removed from atmosphere by photosynthesis

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Oxygen 21%

Produced by photosynthesis in plants and is needed for human and animal respiration

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Water Vapor 0-4%

Varies by region and conditions; acts as a temporary GHG, but less concerning than CO2, quickly cycles through atmosphere

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What is the order of the earth's atmosphere #1

Troposphere: Tropo= change, weather occurs here, 0-16km, most dense due to the pressure of the other layers above it, most of the atmosphere gas molecules are found here, ozone in the troposphere is harmful to humans

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What is the order of the earth's atmosphere #2

Stratosphere: "S" for second, 16-60 km, less dense due to pressure from layers above, thickest O2 layer is found here, absorbs UV-B and UV-C rays which can mutate DNA of animals (cancer)

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What is the order of the earth's atmosphere #3

Mesosphere: Meso= for middle, 60-80km, even less dense

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What is the order of the earth's atmosphere #4

Thermosphere: Them= hottest temp, absorbs harmful X-rays and UV radiation, charges gas molecules glow under intense solar radiation producing northern lights (aurora borealis)

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What is the order of the earth's atmosphere #5

Exosphere: Outermost layer where atmosphere merges with space

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Temperature

Layers of earth's atmosphere are based on where temperature gradients change with distance from earth surface, as you move away from the earth it gets colder, with each layer above it will change from cold to hot

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Troposphere

temperature decreases as the air gets further from the warmth of earth's surface

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Stratosphere

temp increases because top layer of stratosphere is warmed by UV rays (like pool surface)

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Mesosphere

temp decreases because density decreases, leaving fewer molecules to absorb the sun, the coldest place on earth -150 degrees

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Thermosphere

temp increases due to the absorption of highly energetic solar radiation, the hottest place on earth 3,100 degrees

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4.4 takeaways

1. the atmosphere is made of a mix of gases in varying percentages

2. layers of the atmosphere thin out as you travel higher

3. temperature oscillates for various reasons including content and radaiton

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Hadley cell #1

More direct sunlight at the equator warms the air, warm air rises

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Hadley cell #2

Warm air rises, cools, and expands, H20 vapor condenses into rain, warm air holds more moisture than cold

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Hadley cell #3

Air continues to rise, cool, and expand, rising air expands and cools

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Hadley cell #4

Cooling, expanding air spreads out, cool air cant hold as much H2O vapor (condenses and turns into rain)

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Hadley cell #5

Cool, dry air sinks back down to earth at 30 degrees North and South, deserts form here due to lack of moisture in air, after cooling and expanding, air sinks

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Coriolis effect

deflection of objects traveling through atmosphere due to spin of earth

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Coriolis effect air at 30 degrees

moves back to low pressure of equator

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Coriolis effect wind between 0-30 degrees

moves from east to west because earth is spinning west to east

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Coriolis effect wind between 30-60 degrees

moves west to east because earth spins faster at 30 degrees than at 60 degrees

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Global Wind Patterns 0 degrees

Low pressure

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Global Wind Patterns 30 degrees

High pressure

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Global Wind Patterns 60 degrees

Low pressure

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4.5 takeaways

1. winds are driven by certain factors: solar radiation and the Coriolis effect

2. these factors lead to patterns that are predictable

3. wind patterns can lead to patterns in climate and habits at thoes climates