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Material Type: Notes; Class: SKY & SOLAR SYSTEM; Subject: ASTRONOMY & ASTROPHYSICS; University: Iowa State University; Term: Fall 2005;
Typology: Study notes
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General properties: size, orbit, moons
Hemisphere dichotomy
Tharsis Bulge features, volcanos and tectonics
climate changes?
evidence of liquid water
Brief review of last time: Mars
Reading: Chapter 11, Section 11.1-11.3, 11.5-6, (14.3-14.4)
Midterms posted on WebCT: please check with us with grade questions
Observing Session: Tomorrow (if clear - stay tuned to the website)
Jupiter Saturn Uranus
% H 75 85 74
% He 24 14 24
%CH 4 < 0.1 < 0.1 < 1
% NH 3 < 0.1 < 0.1 < 0.
avg. T [C] -150 -185 -
Clouds (^) NH 3 , H 2 O,? NH 3 , NH 4 SH NH 3 , CH 4
Venus Earth Mars
Surf. Pressure 92 1 0.
%CO 2 96 trace 95
%N 2 4 77 3
% O 2 0 21 0
avg. T [C] 470 15 -
Clouds H 2 SO 4 H 2 O CO 2 , H 2 O
Astro 120 Fall 2005: Lecture 16 page (^3)
mostly H 2
, He
av.mol.speed = 2. 1 km/s ×
m h
mmol
1 / 6 vesc = 1. 9 km/s ×
Mplanet
MEarth
REarth
gas will escape if this is greater than 1/6 v esc
Astro 120 Fall 2005: Lecture 16 page (^4)
gas pressure upwards
!!! balances
gravity (weight) downwards
warm if layer absorbs solar energy
cool if layer is transparent to solar radiation
IR absorbers: CO 2 , H 2 O
UV absorbers: N 2 , O 2 , O 3
UV absorption by N 2 , O 2
O 3 great absorber of UV
cold
ground heating
Astro 120 Fall 2005: Lecture 16 page (^7)
solar energy arrives at Earth, heats up ground
ground radiates energy in far–IR
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 2005: Lecture 16 page (^8)