Overview of Planetary Atmospheres - Sky and Solar System | ASTRO 120, Study notes of Astronomy

Material Type: Notes; Class: SKY & SOLAR SYSTEM; Subject: ASTRONOMY & ASTROPHYSICS; University: Iowa State University; Term: Fall 2005;

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Astro 120 Fall 2005: Lecture 16 page 1
Mars
General properties: size, orbit, moons
Hemisphere dichotomy
Tharsis Bulge features, volcanos and tectonics
climate changes?
evidence of liquid water
results from Mars Exploration Rovers
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)
Astro 120 Fall 2005: Lecture 16 page 2
Overview of Planetary Atmospheres
Jupiter
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, NH4 SH
NH3, CH4
Jovians
Venus
Mars
Surf. Pressure
92
0.007
%CO2
96
95
%N2
4
3
% O2
0
0
avg. T [C]
470
-50
Clouds
H2SO4
CO2 , H2O
Terrestrial
Astro 120 Fall 2005: 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 = 2.1 km/s×!T
273K×mh
mmol
1/6vesc = 1.9 km/s×!Mplanet
MEarth
×REarth
R
gas will escape if this is greater than 1/6 vesc:
Astro 120 Fall 2005: Lecture 16 page 4
outgassing (volcanism): release of gas from interior
!!CO2, N2, H2O, CH4, SO2
impacts of icy bodies: H2O, CH4, CO2
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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Mars

General properties: size, orbit, moons

Hemisphere dichotomy

Tharsis Bulge features, volcanos and tectonics

climate changes?

evidence of liquid water

• results from Mars Exploration Rovers

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)

Overview of Planetary Atmospheres

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

J

o

vians

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

T

er

r

estrial

Astro 120 Fall 2005: Lecture 16 page (^3)

Primordial Atmosphere composition:

mostly H 2

, 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

273 K

×

m h

mmol

1 / 6 vesc = 1. 9 km/s ×

Mplanet

MEarth

×

REarth

R

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

Astro 120 Fall 2005: Lecture 16 page (^4)

• outgassing^ (volcanism):^ release of gas from interior

!! CO 2 , N 2 , H 2 O, CH 4 , SO 2

• impacts^ of icy bodies:^ H 2 O,^ CH 4 ,^ CO 2

• chemistry

  • O 2 bound up in oxides (very fast)
  • CO 2 bound up in carbonate rocks,^ surface^ H 2 O
  • H 2 O bound up in rock

• geology

  • H 2 O^ trapped beneath surface (permafrost)

• BIOLOGICAL^ ACTIVITY:

  • photosynthesis:^ CO 2 —>^ O 2 ;^ methane from cows

• Human^ Activity

!! CO 2 , complex organics, CFCs, ozone depletion

Secondary Atmosphere alteration

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

temperature depends on composition of

atmospheric layers as well as pressure and density:

IR absorbers: CO 2 , H 2 O

UV absorbers: N 2 , O 2 , O 3

Atmospheric Pressure and Temperature

Earth’s Atmosphere

80-110 km: thermosphere

UV absorption by N 2 , O 2

50-80 km: mesosphere

O 2 +UV –> O

O + O 2 + UV –> O 3

O 3 great absorber of UV

10-50 km: stratosphere

cold

0-10 km: troposphere

ground heating

• H^2 O

Astro 120 Fall 2005: 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 2005: Lecture 16 page (^8)

The Greenhouse Effect