Lecture 16 - Earth's Atmosphere (11/5/98)


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ASTR11
Reading:

Chapter 4-5, 4-6 (ZG4)


An image of the Aurora Borealis oval from the Polar Spacecraft (courtesy G.E.Parks UWash, NASA)
? Key Question: What determines how high in the atmosphere a particular gas can go?
! Key Principle: Pressure Scale Height
# Key Problem: Calculate the scale height of the atmosphere at sea level.
@ Key Quote:

Investigations:

  1. Atmospheric Composition, Weather and Climate
  2. The Magnetosphere
  3. Structure of Our Atmosphere

Earth's Atmospheric Composition:

Species Abundance (%) Activity
N2 78.1 inert
O2 20.9 active (oxidizing)
Ar 0.93 inert
CO2 0.034 greenhouse, increasing
Ne 0.0028 inert
CH4 0.0005 greenhouse (reducing), increasing
H2O 0.1 - 3 variable

More Telescopes and Interferometers



The Green Bank Telescope under construction in West Virginia as of 19Aug98 (courtesy NRAO)

The Aurora

Some interesting images of the aurora (borealis and australis) can be found on the Web, particularly on the Astronomical Picture of the Day website!

Also note that Jupiter has a much larger magnetic field than the Earth, though it is further from the Sun also. Almost all the gas giants have substantial magnetospheres and show auroral activity!



Jupiter's aurorae as seen by HST (courtesy STSCI/NASA)


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smyers@nrao.edu Steven T. Myers