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structure and composition of the atmosphere structure and composition of the atmosphere

structure and composition of the atmosphere - PowerPoint Presentation

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structure and composition of the atmosphere - PPT Presentation

Objectives Describe the composition of Earths atmosphere Explain why air pressure changes with altitude Explain how air temperature changes with atmospheric composition Describe the layers of the atmosphere ID: 603508

atmosphere temperature layer altitude temperature atmosphere altitude layer air pressure atmospheric troposphere stratosphere increases energy decreases earth

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Slide1

structure and composition of the atmosphereSlide2

Objectives

Describe the composition of Earth’s atmosphere.

Explain why air pressure changes with altitude.

Explain how air temperature changes with atmospheric composition.

Describe the layers of the atmosphere.Slide3

What is the Atmosphere?

View of the atmosphere from the space shuttle

The

atmosphere

is a mixture of gases surrounding EarthSlide4

Composition of the Atmosphere

Nitrogen (78%), the most common atmospheric gas, is released when dead plants and dead animals break down and also when volcanoes erupt.

Oxygen (21%), the second most common atmospheric gas, is made by producers.

The remaining 1% of the atmosphere is made up of argon, carbon dioxide, water vapor and other gases.Slide5

Atmospheric Pressure

Atmospheric pressure is the amount of force or pressure exerted by the atmosphere on the objects located within it.

When it is pressing down with more force, we say that it is a high pressure.

When the atmosphere presses in with less force, we say that there is a low pressure in the area.Slide6

Atmospheric Pressure

The atmosphere is held around the Earth by gravity.

Gravity pulls gas molecules in the atmosphere toward the Earth’s surface, causing air pressure.

As altitude increases, the force of gravity decreases and so air pressure decreases.Slide7

Atmosphere & Temperature

Differences in atmospheric temperatures are

the

result of the

way solar energy is absorbed by the different gases present and the density of those gases.

As the altitude increases the number of air molecules decreases, thus the average of their kinetic energy decreases. The results is a decrease in air temperature with an increase of altitude

.Slide8

Layers of the Atmosphere

The Earth’s atmosphere is divided into four layers based on

temperature

.

The name of each layer gives you clues about its features:

Troposphere

(

tropo

= turning or change)

Stratosphere

(

strato

= layer)

Mesosphere

(

meso

= middle)

Thermosphere

(

thermo

= heat)Slide9
Slide10
Slide11

Troposphere

Lowest layer of the atmosphere, from Earth’s surface to about 10 km above.

Temperature decreases with altitude.

Contains almost 90% of the atmosphere’s mass.

Nearly all weather occurs in this layer.

The zone known as the

tropopause

represents the upper boundary of the troposphere.Slide12

Stratosphere

The atmospheric layer above the troposphere.

Lower stratosphere is extremely cold, but temperature increases as altitude increases in the stratosphere.

Rises because

ozone

, (O

3

), in the stratosphere absorbs UV radiation from the sun, warming the air

 protects life on Earth.Slide13

Stratosphere

This increase in temperature with height means warmer air is located above cooler air. This is the reason for the 'anvil-shaped' tops of cumulonimbus clouds.

The zone known as the

stratopause

represents the upper boundary of the stratosphere.

 Slide14

Mesosphere

The middle layer of the atmosphere.

From 50km-80km above the earth’s surface.

Coldest layer.

Temperature decreases as altitude increases, just like the troposphere.

Meteorites

and space dust burn up in this layer.

The zone known as the

mesopause

represents the upper boundary of the mesosphere.Slide15

Thermosphere

Uppermost atmospheric layer.

From 80km – 480km above the earth’s surface.

Temperature again increases steadily with altitude because nitrogen and oxygen atoms absorb solar radiation.

Contains a special part called the

ionosphereSlide16

Temps in the Troposphere & Thermosphere

Although the thermosphere has very high temperatures, IT DOES NOT FEEL HOT.

Heat is different from temperature.

Heat IS energy, which is about particles in MOTION.

Temperature is a MEASURE of the average energy in substance.

Heat energy depends on the speed, size and type of particle. Temperature does not.

For example, the temperature of a small cup of water might be the same as the temperature of a large tub of water, but the tub of water has more heat because it has more water and thus more total thermal energy.Slide17

Troposphere

ThermosphereSlide18

Ionosphere

The lower part of the thermosphere

Defined based on electrical characteristics within the thermosphere

absorbs cosmic rays, gamma rays, X-rays, some UV rays

contains ions: charged electrical particles

visible light is emitted when ions are bombarded by cosmic radiation

produce aurora borealis, aurora

australis

Slide19

Review

Why does temperature decrease with altitude in the troposphere?

Why does temperature

increase with

altitude in the

stratosphere? Why does temperature decrease with altitude in the

mesosphere?