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34 Cards in this Set

  • Front
  • Back

Original atmosphere

Primarily helium and hydrogen destroyed by the solar wind of the sun.

Second atmosphere

Formed 4.4 billion years ago Contained mainly Carbon Dioxide and water vapor with some nitrogen and no oxygen.100 times more gas than current atmosphere.Carbon dioxide was dissolved in the seas and created carbonates.

About 3.3 million years ago the first oxygen producing organisms (cyanobacteria) appeared.

Responsible for adding oxygen to the atmosphere.Ozone was formed and provided protection to organisms from the ultraviolet radiation.Nitrogen levels started to increase from the breakdown of ammonia by sunlight and bacteria.

Third atmosphere

Was formed 200-250 million years ago and evolved to the current atmosphere.

Nitrogen

78%Needed to produce proteinReturned to the atmosphere by the decaying of plants and animals

Oxygen

21%Needed for respiration and combustionReturned to the atmosphere

Carbon Dioxide

Small amount found in atmosphereUsed by plants to make food photosynthesisReturned to the atmosphere by the respiration of plants and animals Water VaporPlays an important role in earth’s weather

Ozone

Made up of 3 oxygen moleculesProtects us from ultraviolet radiation

Dust Particles

needed for water vapor to condense

Atmospheric Pressure

The force exerted on a surface by the weight of the air above that surface.

99% of the total mass of atmospheric gases is found within 32 km of the surface 1 cm column of air, at sea level, has a mass of 1.03 kg or 2 lbs. (14.7 pounds per square inch at sea level)

Atmospheric pressure decreases as altitude increases.Air Pressure is equal in all directionsAtmospheric pressure is depended upon the density of air

Measuring Atmospheric Pressure

Units used to measure pressure are inches, centimeters, and millibars

Lowest in inches, centimeters, and or millibars

the Lowest was 25.69 inches

Highest in inches, centimeters, and or millibars

Highest sea level pressure was 32.06 inches

Factors that affect air pressure/ Density

Water Vapor


Temperature


Elevation

How does water vapor affect air pressure?

Large amounts of water vapor cause lower air pressure

How does temperature affect air pressure?

Warmer is less dense, causing lower ai pressure

How does elevation affect air pressure?

Air becomes less dense(thinner) at higher altitudes causing lower air pressure

Types of air pressure

Low Pressure


High Pressure

What is high pressure?

Cool and dry air


Rotate Clockwise


Clear and sunny weather

What is low pressure?

Warmer air and humid air


Rotate Counter-clockwise


Inclement weather

Barometer

Instrument used to measure air pressure

Mercurial Barometer

Consists of a glass column standing in a well of mercury. As air pushes down on the mercury, the height of the mercury will rise or fall in the glass column

Aneroid Barometer

Consist of sealed metal container free of air. As air pressure changes, the container expands or contracts. A moving pointer on a scale indicates these changes.Increased air pressure causes the container to bend in.This is the most common type of barometer

Wind

Air in motion movement from one point to another

What direction does wind Travel in?

High to low

Wind Characteristics.

Causes Changes in atmospheric pressure


Movement Air flows from high pressure to low pressure High pressure air is cool and denseLow pressure air is warm and less dense

Naming of Winds

Winds are named according to the direction they come from

Measuring and Detecting Winds

Wind vane: points to where the wind is coming fromWind Speed


Anemometer: Measures speed in mph or knots

Types of Atmospheres

Ionosphere


Exosphere


Mesosphere


Ozone

Ionosphere

Lower region of thermospherere flects radio waves

Exosphere

upper region of thermosphere

Mesosphere

coldest layer

Ozone

made of 3 molecules of oxygen