Lecture 6 6/11/07 Ast 1001. Earth’s Atmosphere The Earth’s atmosphere has several very important...

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Lecture 6 6/11/07 Ast 1001

Transcript of Lecture 6 6/11/07 Ast 1001. Earth’s Atmosphere The Earth’s atmosphere has several very important...

Page 1: Lecture 6 6/11/07 Ast 1001. Earth’s Atmosphere The Earth’s atmosphere has several very important properties: –Just enough warmth –Just enough pressure.

Lecture 6

6/11/07

Ast 1001

Page 2: Lecture 6 6/11/07 Ast 1001. Earth’s Atmosphere The Earth’s atmosphere has several very important properties: –Just enough warmth –Just enough pressure.

Earth’s Atmosphere

• The Earth’s atmosphere has several very important properties:– Just enough warmth– Just enough pressure– Water can exist in three phases– Protects us from solar radiation– Allows for weather

Page 3: Lecture 6 6/11/07 Ast 1001. Earth’s Atmosphere The Earth’s atmosphere has several very important properties: –Just enough warmth –Just enough pressure.

The Big Questions

• Why did Earth retain most of its outgassed water?

• Why does Earth have so little carbon dioxide compared to Venus?

• Why does Earth have so much Nitrogen and Oxygen?

• Why does Earth have a UV absorbing stratosphere?

Page 4: Lecture 6 6/11/07 Ast 1001. Earth’s Atmosphere The Earth’s atmosphere has several very important properties: –Just enough warmth –Just enough pressure.

Water and Carbon Dioxide

• Temps were low enough for water vapor to condense– Earth had oceans 4.3 billion years ago

• Ocean’s explain why there is so little carbon dioxide in atmosphere– Most of the carbon dioxide dissolved into the

oceans

Page 5: Lecture 6 6/11/07 Ast 1001. Earth’s Atmosphere The Earth’s atmosphere has several very important properties: –Just enough warmth –Just enough pressure.

Nitrogen and Oxygen

• We have so much nitrogen because it isn’t absorbed as much as carbon dioxide

• Life is key to explaining why we have so much oxygen– Oxygen breaks down after several millions of

years– Also explains why we have an ozone layer

Page 6: Lecture 6 6/11/07 Ast 1001. Earth’s Atmosphere The Earth’s atmosphere has several very important properties: –Just enough warmth –Just enough pressure.

Earth’s Stable Climate

• Earth has a relatively stable climate• Earth self regulates via the carbon dioxide cycle

– Atmospheric carbon dioxide dissolve into rainwater

– Rain erodes the rocks, bringing minerals to the oceans

– Calcium combines with carbon dioxide and makes rocks like limestone

– Plate tectonics carry the rocks to the subduction zone

– Rock melts and releases its carbon dioxide back into the atmosphere through volcanoes

Page 7: Lecture 6 6/11/07 Ast 1001. Earth’s Atmosphere The Earth’s atmosphere has several very important properties: –Just enough warmth –Just enough pressure.

Feedback• What if Earth warms up?

– More evaporation and rainfall

– More carbon dioxide out of the atmosphere

– Weaker greenhouse effect

• What if Earth cools down?– Less rainfall– More carbon dioxide in the

atmosphere– Stronger greenhouse effect

Page 8: Lecture 6 6/11/07 Ast 1001. Earth’s Atmosphere The Earth’s atmosphere has several very important properties: –Just enough warmth –Just enough pressure.

Long Term Change• It takes the carbon dioxide

cycle time to stabilize the temps– We can have ice ages or hot

spells

– Geologists have discovered a snowball Earth phase

• Eventually the gradually brightening Sun will cause major climate issues

Page 9: Lecture 6 6/11/07 Ast 1001. Earth’s Atmosphere The Earth’s atmosphere has several very important properties: –Just enough warmth –Just enough pressure.

Humans and Climate

• It is undeniable that humans affect climate and our planet– Ozone layer hole– Mass extinctions

Page 10: Lecture 6 6/11/07 Ast 1001. Earth’s Atmosphere The Earth’s atmosphere has several very important properties: –Just enough warmth –Just enough pressure.

Global Warming• There is controversy about how

serious the problem is, but the following facts are clear:– Measurements show that the Earth

has warmed over the past 50 years

– The burning of fossil fuels and other human activity dumps greenhouse gasses into the atmosphere

– Eventually, a continually rising concentration of greenhouse gasses would make our planet warm up