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Earth’s Atmosphere

Date post: 07-Feb-2016
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Earth’s Atmosphere. What newsworthy weather events have you noticed in the media?. Weatherbug. http://achieve.weatherbug.com/Home.aspx#target1 http://www.wnep.com/weather/regionaldoppleriiradar/. Can you describe what you see in this picture?. - PowerPoint PPT Presentation
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Earth’s Atmosphere
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Page 1: Earth’s Atmosphere

Earth’s Atmosphere

Page 2: Earth’s Atmosphere

What newsworthy weather events have you noticed in the media?

Page 3: Earth’s Atmosphere

Weatherbug

• http://achieve.weatherbug.com/Home.aspx#target1

• http://www.wnep.com/weather/regionaldoppleriiradar/

Page 4: Earth’s Atmosphere

Can you describe what you see in this picture?

In this chapter you will learn about Earth’s atmosphere, and the gases that support life.

Page 5: Earth’s Atmosphere

Size of the Earth

• 1. Diameter = from the north pole to the south pole it’s ~ 7916 miles

• 2. Circumference ~ 24,901 miles

• Equator- imaginary line that divides the earth into hemisphere’s (north and south)

Page 6: Earth’s Atmosphere
Page 7: Earth’s Atmosphere

Tell the person next to you what the 3 most important features of earth• 1. land lithosphere

• 2. air atmosphere

• 3. water hydrosphere

Page 8: Earth’s Atmosphere

Viking---astronomy connection

Page 9: Earth’s Atmosphere

Past Atmosphere 4 billion yrs ago

Methane

Ammonia

Water

5-2 Development of Earths atmosphere

Page 10: Earth’s Atmosphere

Atmosphere at 3.8 billion yrs. old

Methane

Methane

Methane

Ammonia

Ammoniawater

hydrogen

Carbon dioxide

nitrogenwaterwater

New gases

Page 11: Earth’s Atmosphere

Water

water

water water

water

H20

H 00 0

0HH

Ozone= 3 oxygen atoms combined together to form a protective layer

Page 12: Earth’s Atmosphere

• Due to the ozone• Blue-green bacteria

started to become more abundant

• used sunlight, carbon dioxide (co2) and water to make food, their byproduct was oxygen

Page 13: Earth’s Atmosphere

Present Atmosphere

Page 14: Earth’s Atmosphere

5-3 Layers of the Atmosphere

What do mountain climbs have to carry as they climb higher into the atmosphere?

Page 15: Earth’s Atmosphere

La Rinconada, Peru

Page 16: Earth’s Atmosphere
Page 17: Earth’s Atmosphere

Layers of the atmosphere depends on temperature changes

Page 18: Earth’s Atmosphere

Troposphere

11 mi.

31mi.56 mi.

1.Almost all weather occurs here

2. Extends 11miles high

3. Jet stream

Page 19: Earth’s Atmosphere

Convection currents

Currents of air are produced as warm air rises and cool air replaces it.

Page 20: Earth’s Atmosphere

Convection currents

• Movement of air caused by a difference in temperature

• What’s really happening• Cool dense air is sinking and warm, less dense

air is rising, causing a movement of air

Page 21: Earth’s Atmosphere

Stratosphere

• Lower stratosphere temp. = extremely cold

Page 22: Earth’s Atmosphere

Stratosphere

• Jet stream winds- strong eastward wind that blows horizontally around the earth

Page 23: Earth’s Atmosphere

Stratosphere

• Ozone layer

Cold = -76°f

Warm = 64° f

• Ozone ( a form of oxygen, O3) reacts with the uv light to warm the air

• Protects earth from harmful uv radiation

Page 24: Earth’s Atmosphere

Stratosphere

Temperatures increase as you ascend. Why?The Ozone Layer absorbs ultraviolet rays,

giving off heat.The Jet Stream

Page 25: Earth’s Atmosphere

Video-15 min

• http://www.youtube.com/watch?v=L4CX7GL_DPo

Page 26: Earth’s Atmosphere

Mesospherecoldest area of the

atmosphereShooting Stars-

what are they?• Protect us from

falling meteoroids

Page 27: Earth’s Atmosphere

Meteoroids, meteors and meteorites

• Meteoroid: An object in space no smaller than a speck of dust and no larger than an asteroid. Most are thought by scientists to be pieces of asteroids or comets.

• Meteor: The streak of light that forms when a meteoroid burns while traveling at high speed through Earth's atmosphere (a "shooting star" or "falling star").

• Meteorite: The remnants of a meteoroid that has passed through the atmosphere and struck the Earth.

Page 28: Earth’s Atmosphere

Thermosphere

• No definite Limit• Very Hot? Why

• Nitrogen and Oxygen absorb a lot of UV radiation and convert it to heat

• Thin air makes seeing objects in space more easily.

Page 29: Earth’s Atmosphere

Ionosphere• Lower layer of the thermosphere• Gas molecules are electrically charged

• Radio waves bounce back• Brilliant light displays of aurora borealis

occur here

Page 30: Earth’s Atmosphere

Thermosphere

• No definite upper limit

• Outer layer of thermosphere• Satellites orbit Earth here

• Communicate long-distance telephone and television signals

• Watch weather and weather patterns

Exosphere

Page 31: Earth’s Atmosphere

Magnetosphere• Extends above Earth • Magnetic field that traps charged particles

from the sun• Particles follow the lines of magnetic force

and bounce back and forth from one pole to the other• Sometimes breaking through into the

ionosphere to produce auroras

Page 32: Earth’s Atmosphere

Aurora Borealis, Northern Lights

Page 33: Earth’s Atmosphere

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