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Meteorology.

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Presentation on theme: "Meteorology."— Presentation transcript:

1 Meteorology

2 What is the Atmosphere? Mixture of gases that surround the Earth.
Composition 78% Nitrogen 21% Oxygen 1%: other argon, carbon dioxide What is the purpose of the atmosphere? Makes conditions suitable for us to live Protects us from space

3 What is the Atmosphere: continued
Why is it Important? Stores Oxygen Keeps us warm: Greenhouse effect Protects us from sun’s radiation, cold of space, meteoroids

4 Air Pressure Does air have mass?
How could you prove/demonstrate that air has mass? Measure of force with which air molecules push on a surface Air pushes in all directions Gases will fill the volume of space they are contained Density of air effects the amount of pressure, why? How is pressure measured?

5 Altitude and Air pressure
Altitude = Elevation Air pressure decreases as altitude increases Air pressure decreases, density decreases

6 Layers of Atmosphere 4 main layers Troposphere Stratosphere Mesosphere
Thermosphere

7 Troposphere Tropo = Change Layer in which we live Weather occurs here
What is the difference between weather and climate? Majority of mass of atmosphere Altitude increases, temperature decreases Top temp. = -60 degrees Celsius 0 to 12 km

8 Stratosphere Contains the Ozone
What is ozone? 3 oxygen molecules bonded together Top of Stratosphere is warm, but bottom is cold, Why? Ozone absorbs Suns radiation Ranges from 12km to 50 in elevation

9 Mesosphere Layer protects us from meteoroids and space junk
Meteoroids burn up = Shooting stars

10 Thermosphere Divided into 2 layers Outermost layer of atmosphere
Exosphere Ionosphere Outermost layer of atmosphere Temp can reach up to 1,800°C Suns radiation strikes this layer first Thermometer would read 0°C, Why? Density and distance between molecules. Molecules have a lot of energy but there isn’t a lot of molecules and they are spread out Temperature = Average amount of energy of motion of each particle

11 Thermosphere: Ionosphere
Sun’s energy innervates gas molecules to become electrically charged Ions We see this as Auroa Borealis: Northern Lights Layers reflects back radio waves

12 Thermosphere: Exosphere
400 km and beyond Layer in which satellites orbit Earth


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