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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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Astro 120 Fall 2003: Lecture 16 page 1
recent and continued volcanic activity
strange features: arachnoids, coronae,...
overwhelming atmosphere
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
Text
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
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
Astro 120 Fall 2003: Lecture 16 page 3
mostly H
, He
trace elements tied up in molecules
av
mol
speed = 2
1 km
s ×
m
h
m
mol
v esc
9 km
s (^) ×
planet
Earth
Earth R
gas will escape if this is greater than 1/6 v
esc
Astro 120 Fall 2003: Lecture 16 page 4
bound up in oxides (very fast)
bound up in carbonate rocks, surface H
O bound up in rock
O trapped beneath surface (permafrost)
photosynthesis: CO
; methane from cows
Astro 120 Fall 2003: Lecture 16 page 5
gas pressure upwards
balances
density also highest at surface, drops with altitude
warm if layer absorbs solar energy
cool if layer is transparent to solar radiation
IR absorbers: CO
UV absorbers: N
Astro 120 Fall 2003: Lecture 16 page 6
UV absorption by N
great absorber of UV
cold
ground heating
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
some gasses are transparent in visible/UV wavelengths
but
are opaque (absorbers) in the Infrared
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