Astro 120 Fall 2003: Lecture 16 - Planetary Atmospheres and Greenhouse Effects, Study notes of Astronomy

A portion of lecture notes from astro 120 fall 2003, lecture 16. The notes cover the topics of planetary atmospheres, their compositions, and the greenhouse effect. The lecture discusses various planets, including venus, mars, jupiter, saturn, uranus, and earth, and their atmospheric features, such as temperature structures, hydrostatic equilibrium, and thermal equilibrium.

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Uploaded on 09/02/2009

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Astro 120 Fall 2003: Lecture 16 page 1
Venus
recent and continued volcanic activity
strange features: arachnoids, coronae, . . .
overwhelming atmosphere
Mars
Hemisphere dichotomy
Tharsis Bulge features
polar caps
evidence of liquid water
Brief review of last time: Venus and Mars
Reading: Chapter 11, Section 11.1-11.3, 11.5-6, (14.3-14.4)
Midterms submitted: please check with us with grade questions
Astro 120 Fall 2003: Lecture 16 page 2
Overview of Planetar
y
Atmos
p
heres
Text
J
u
p
iter Saturn Uranus
% H 75 85 74
% He 24 14 24
%CH4< 0.1 < 0.1 < 1
% NH3< 0.1 < 0.1 < 0.1
avg. T [C] -150 -185 -210
Clouds NH3, H2O, ? NH3, NH4SH NH3, C H 4
Jovians
Venus Earth Mars
Surf. Pressure 92 1 0.007
%CO296 trace 95
%N2477 3
% O2021 0
avg. T [C] 470 15 -50
Clouds H2SO4H2OCO
2 , H2O
Terrestrial
Astro 120 Fall 2003: Lecture 16 page 3
Primordial Atmosphere composition:
mostly H2, He
trace elements tied up in molecules
CO2, CH4, N2, H2O, NH3
Hydrogen largely lost from inner planets very early:
Planetary Atmospheres: gas, vapor, ice
av.mol.speed = 2.1km/s×T
273K×mh
mmol
1/6vesc =1.9km/s×Mplanet
MEarth
×REarth
R
gas will escape if this is greater than 1/6 vesc:
Astro 120 Fall 2003: Lecture 16 page 4
outgassing (volcanism): release of gas from interior
CO2, N2, H2O, CH4, S O 2
impacts of icy bodies: H2O, CH4, C O 2
chemistry
O2 bound up in oxides (very fast)
CO2 bound up in carbonate rocks, surface H2O
H2O bound up in rock
geology
H2O trapped beneath surface (permafrost)
BIOLOGICAL ACTIVITY:
photosynthesis: CO2 —> O2; methane from cows
Human Activity
CO2, complex organics, CFCs, ozone depletion
Secondary Atmosphere alteration
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Astro 120 Fall 2003: Lecture 16 page 1

• Venus

recent and continued volcanic activity

strange features: arachnoids, coronae,...

overwhelming atmosphere

• Mars

Hemisphere dichotomy

Tharsis Bulge features

polar caps

evidence of liquid water

Brief review of last time:

Venus and Mars

Midterms submitted: please check with us with grade questions Reading: Chapter 11, Section 11.1-11.3, 11.5-6, (14.3-14.4)

Astro 120 Fall 2003: Lecture 16 page 2

Overview of Planetary Atmospheres

Text

J

upiter

Saturn

Uranus

% H

% He

%CH

4

% NH

3

avg. T [C]

Clouds

NH

3 , H

2 O,?

NH

3 , NH

4 SH

NH

3 , CH

4

Jovians

Venus

Earth

Mars

Surf. Pressure

%CO

2

trace

%N

2

% O

2

avg. T [C]

Clouds

H 2 SO

4

H 2 O

CO

2 , H

2 O

Terrestrial

Astro 120 Fall 2003: Lecture 16 page 3

• Primordial Atmosphere composition:

mostly H

, He

trace elements tied up in molecules

CO

, CH

, N

, H

O, NH

Hydrogen largely lost from inner planets very early:

Planetary Atmospheres

gas, vapor, ice

av

mol

speed = 2

1 km

s ×

T

K

×

m

h

m

mol

v esc

9 km

s (^) ×

M^

planet

M

Earth

×

R

Earth R

gas will escape if this is greater than 1/6 v

esc

Astro 120 Fall 2003: Lecture 16 page 4

outgassing (volcanism): release of gas from interior

CO

, N

, H

O, CH

, SO

impacts of icy bodies:

H

O, CH

, CO

chemistry

O

bound up in oxides (very fast)

CO

bound up in carbonate rocks, surface H

O

H

O bound up in rock

geology

H

O trapped beneath surface (permafrost)

BIOLOGICAL ACTIVITY:

photosynthesis: CO

—> O

; methane from cows

Human Activity

CO

, complex organics, CFCs, ozone depletion

Secondary Atmosphere alteration

Astro 120 Fall 2003: Lecture 16 page 5

• Pressure vs. height: Hydrostatic Equilibrium:

gas pressure upwards

balances

  • gravity (weight) downwards pressure highest at surface, drops with altitude

density also highest at surface, drops with altitude

• Temperature vs. height: thermal equilibrium:

warm if layer absorbs solar energy

cool if layer is transparent to solar radiation

• atmospheric layers as well as pressure and density:temperature depends on composition of

IR absorbers: CO

, H

O

UV absorbers: N

, O

, O

Atmospheric Pressure and Temperature

Astro 120 Fall 2003: Lecture 16 page 6

Earth’s Atmosphere

80-110 km: thermosphere

UV absorption by N

, O

50-80 km: mesosphere

O

+UV –> O

O + O

+ UV –> O

O

great absorber of UV

10-50 km: stratosphere

cold

0-10 km: troposphere

ground heating

H

O absorbs IR

Astro 120 Fall 2003: Lecture 16 page 7

solar energy arrives at Earth, heats up ground

ground radiates energy in far–IR

far–IR trapped by Greenhouse gasses

ground heats up more, radiates in near–IR

greenhouse gasses allow near–IR to escape sets up a balance with incoming energy

The Greenhouse Effect:

some gasses are transparent in visible/UV wavelengths

but

are opaque (absorbers) in the Infrared

MAIN GREENHOUSE GASSES: CO

, H

O

w/o atmosphere

with atmosphere

Mercury

160 C

160 C

Venus

40 C

470 C

Earth

0 C

15 C

Mars

-55 C

-50 C

Astro 120 Fall 2003: Lecture 16 page 8

The Greenhouse Effect