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Global Warming and the Venus Greenhouse Effect 24 February 2015

Global Warming and the Venus Greenhouse Effect 24 February 2015

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Page 1: Global Warming and the Venus Greenhouse Effect 24 February 2015

Global Warming and the Venus Greenhouse Effect

24 February 2015

Page 2: Global Warming and the Venus Greenhouse Effect 24 February 2015

Venus: Global warming gone bad

Page 3: Global Warming and the Venus Greenhouse Effect 24 February 2015

Earth & Venus: Sister planets?

Venus Earth

Mass 5x1024 kg 6x1024 kg

a (semi-major axis)

0.7 AU 1 AU

T at surface ~750 K ~300 K

P at surface ~90 atm ~1 atm

atm composition

N2 and H2O clouds

CO2 and H2SO4 clouds

What is the boiling Temp of water?

Page 4: Global Warming and the Venus Greenhouse Effect 24 February 2015

© 2014 Pearson Education, Inc.

Table 10.1

Terrestrial Planet Atmospheres

Page 5: Global Warming and the Venus Greenhouse Effect 24 February 2015

How do we know Venus’s surface temperature?

Page 6: Global Warming and the Venus Greenhouse Effect 24 February 2015

How do we know Venus’s surface temperature?

high energy

short wavelength

“bluer”

hot

low energy

long wavelength

“redder”

cold

Page 7: Global Warming and the Venus Greenhouse Effect 24 February 2015

How do we know Venus’s surface temperature?

Earth emits light here. T=300 K

the Sun emits light here. T=6000 K

Venus emits light here. T=750

Page 8: Global Warming and the Venus Greenhouse Effect 24 February 2015

How do we know what the clouds are made of?

Wavelength of light (in the infrared)

Am

ount

of l

ight

obs

erve

d ab

ove

the

atm

osph

ere

Spectrum of planet with no atmosphere

Page 9: Global Warming and the Venus Greenhouse Effect 24 February 2015

How do we know what the clouds are made of?

Wavelength of light (in the infrared)

Wavelength of light (in the infrared)

Am

ount

of l

ight

obs

erve

d ab

ove

the

atm

osph

ere

Am

ount

of l

ight

obs

erve

d ab

ove

the

atm

osph

ere

Wavelength at which a molecule in the atmosphere absorbs light

Spectrum of planet with no atmosphere

Spectrum of planet with atmosphere

Page 10: Global Warming and the Venus Greenhouse Effect 24 February 2015

How do we know what the clouds are made of?

(Infrared light)

Page 11: Global Warming and the Venus Greenhouse Effect 24 February 2015
Page 12: Global Warming and the Venus Greenhouse Effect 24 February 2015
Page 13: Global Warming and the Venus Greenhouse Effect 24 February 2015
Page 14: Global Warming and the Venus Greenhouse Effect 24 February 2015

© 2014 Pearson Education, Inc.

Figure 10.31

Two views:Venusatmosphere

Page 15: Global Warming and the Venus Greenhouse Effect 24 February 2015
Page 16: Global Warming and the Venus Greenhouse Effect 24 February 2015

© 2014 Pearson Education, Inc.

Table 10.2

Page 17: Global Warming and the Venus Greenhouse Effect 24 February 2015

© 2014 Pearson Education, Inc.

Figure 10.18

Climate change causes

Page 18: Global Warming and the Venus Greenhouse Effect 24 February 2015

© 2014 Pearson Education, Inc.

Figure 10.18.1

Page 19: Global Warming and the Venus Greenhouse Effect 24 February 2015

© 2014 Pearson Education, Inc.

Figure 10.18.3

Page 20: Global Warming and the Venus Greenhouse Effect 24 February 2015

© 2014 Pearson Education, Inc.

Figure 10.18.4

Page 21: Global Warming and the Venus Greenhouse Effect 24 February 2015

© 2014 Pearson Education, Inc.

Figure 10.21

Page 22: Global Warming and the Venus Greenhouse Effect 24 February 2015

© 2014 Pearson Education, Inc.

Figure 10.37

Global warming since 1880

Page 23: Global Warming and the Venus Greenhouse Effect 24 February 2015

© 2014 Pearson Education, Inc.

Figure 10.38

CO2 over last 800,000 years

Page 24: Global Warming and the Venus Greenhouse Effect 24 February 2015

© 2014 Pearson Education, Inc.

Figure 10.39

Page 25: Global Warming and the Venus Greenhouse Effect 24 February 2015

© 2014 Pearson Education, Inc.

Figure 10.41

Pink: Melting ice in Greenland!

Page 26: Global Warming and the Venus Greenhouse Effect 24 February 2015

How did Venus get so hot?

Remember - all gases absorb light at specific wavelengths.

“Greenhouse” gases (like carbon dioxide, water and methane) like to absorb in the infrared wavelengths.

Planets emit light at infrared wavelengths (same as human bodies).

Conclusion? “Greenhouse” gases don’t lett the heat from the planet escape.

Page 27: Global Warming and the Venus Greenhouse Effect 24 February 2015

How did Venus get so hot?

Planetary surface

A planet with no atmosphere

Solar radiation comes in

Planetary radiation goes out

Page 28: Global Warming and the Venus Greenhouse Effect 24 February 2015

How did Venus get so hot?

Planetary surface

A planet with an atmosphere

Solar radiation comes in

Planetary radiation goes out, but gets absorbed

The greenhouse gases reradiate. Some of the energy goes towards the surface.

Greenhouse gases

Page 29: Global Warming and the Venus Greenhouse Effect 24 February 2015

How do greenhouse gases get into the atmosphere?

Water: evaporation

CO2: vaporization of rocks, release from traps, vaporization of biotic material (like fossil fuels), respiration

Methane: release from traps, biology (bacteria, cows, rice)

Page 30: Global Warming and the Venus Greenhouse Effect 24 February 2015

Venus is an example of a “runaway greenhouse”.

rocks and water vaporize and release greenhouse gases

greenhouse gases heat the surface of the planet

Why was Venus hot in the first place?

Page 31: Global Warming and the Venus Greenhouse Effect 24 February 2015

Earth was also a “runaway greenhouse” at one point!

rocks and water vaporize and release greenhouse gases

greenhouse gases heat the surface of the planet

Page 32: Global Warming and the Venus Greenhouse Effect 24 February 2015

Why did the Earth cool, but Venus stay so hot?

Page 33: Global Warming and the Venus Greenhouse Effect 24 February 2015

© 2014 Pearson Education, Inc.

Figure 10.32

Page 34: Global Warming and the Venus Greenhouse Effect 24 February 2015

Why did the Earth cool, but Venus stay so hot?

Ideas: Oceans?

Biology?

It probably has to do with water, but why the Earth has water and Venus doesn’t is not well

understood. It MAY be that water allowed plate tectonics to occur, and when the oceanic plates

subduct, they take CO2 with them.

Page 35: Global Warming and the Venus Greenhouse Effect 24 February 2015

© 2014 Pearson Education, Inc.

Page 36: Global Warming and the Venus Greenhouse Effect 24 February 2015

The Surface of Venus

Venus’s surface can’t be viewed in visible light. The atmosphere absorbs most visible light.

Radio light reaches the surface.

Page 37: Global Warming and the Venus Greenhouse Effect 24 February 2015

Venus’s surface was mapped with RADAR.

surface

RADAR instrument

RADAR instruments can map topography.

Page 38: Global Warming and the Venus Greenhouse Effect 24 February 2015

Venus’s surface was mapped with RADAR.

smooth surface

RADAR instrument

RADAR instruments can determine roughness.

rough surface

Page 39: Global Warming and the Venus Greenhouse Effect 24 February 2015

Venus’s surface was mapped with RADAR.

Reflective surface

RADAR instrument

RADAR instruments can determine reflectivity.

Absorptive surface

Page 40: Global Warming and the Venus Greenhouse Effect 24 February 2015

Venus’s has few small craters. Why?

Venus’s has few large craters. Why?

Page 41: Global Warming and the Venus Greenhouse Effect 24 February 2015

Venus’s has few small craters. Why?

Venus’s has few large craters. Why?

Venus has a dense atmosphere.

Venus’s surface is ‘young’.

Page 42: Global Warming and the Venus Greenhouse Effect 24 February 2015

How are craters on Venus different from craters on other bodies?

Venusthe moon

Page 43: Global Warming and the Venus Greenhouse Effect 24 February 2015

Venus’s surface is covered with volcanic features.

How can you tell impact craters from volcanic calderas?

What does the brightness mean in these images?

Page 44: Global Warming and the Venus Greenhouse Effect 24 February 2015

Venus’s surface is covered with volcanic features.

Few craters have been altered by lava.

What does this mean?

If lava lies over an existing crater, then the crater came first.

Page 45: Global Warming and the Venus Greenhouse Effect 24 February 2015
Page 46: Global Warming and the Venus Greenhouse Effect 24 February 2015

Venus: Take-away messages

•Venus’s bulk properties (mass, size, distance from sun) are similar to Earth.

•However, Venus’s atmosphere has a lot of CO2 and therefore its surface is very hot.

•Exactly why Venus and Earth evolved in different ways is not well understood, but is probably related to water.

•Volcanism is an important process on its surface, but may not have been active recently.

•Venus’s entire surface is ‘young’, so some global resurfacing event occurred.