"Reach for the Stars" Solutions, Division C

65 points total

Part I: Star ID section (25 pts):
 

Part II: Knowledge Tasks (35 pts):

The asteroid belt. There is not enough gravity to hold the gases in place during the hottest part of the day. The Sun illuminates a different 50% of the Moon than the 50% that Earth sees. The part that overlaps is the part that we see illuminated from Earth at any particular phase. Parallax. By using triangulation and observing the nearby stars from different positions along Earth's orbit we can calculate the distance to the object with simple geometry. The Main Sequence. The star is bigger. Stars in the upper right corner of the H-R diagram are "Giants" thus, even though each square meter of surface my radiate less light, there is a LOT more surface area. White dwarf. These are located in the bottom left corner of the H-R diagram. They are "changing fuel." I.e., They are changing from hydrogen fusion to helium fusion. Because of the different temperatures and volumes involved the star is unstable until it adjusts to the new fuel. The plane of the Moon's orbit is tilted by 5 from the plane of Earth's orbit. Since the Moon is only 0.5 wide, most of the time it is either too high or too low to be in Earth's shadow. Star "B" is further away by a factor of 2. Because of the 1/r2 drop off of light intensity, doubling the distance decreases the brightness by a factor of 4. 2.5 times. The 1st Magnitude star is brighter. By using blackbody radiation. We measure the continuous spectrum of the star and determine which color (wavelength) is brightest. From That we can determine the temperature of the star. By Wien's law: (max. wavelength in nm) = 2.9×106 / (T in Kelvin) wavelength = 500 nm. Strong radio and x-ray emissions, jets of matter ejected, and/or enormous orbital velocities (as measured by the Doppler red shift and blue shift) of the stars near the core as measured by Kepler's and Newton's laws. Earth's axis is tilted relative to the plane of the orbit. Thus in winter the sunlight strikes Earth at an oblique angle which spreads out the light over more surface area - the light is less intense. Also, the tilt of the axis causes the days to be shorter in winter. Hence we have both weaker light and less time in that light to warm the surface. In summer the reverse is true. Sidereal time is time measured relative to the stars rather than the Sun. (A sidereal day is about 4 minutes shorter than a mean solar day.) The current local sidereal time is exactly equal to the right ascension of any star that happens to be on the meridian (line from north to south through the overhead point, or zenith) at that moment.

(The last three problems have been removed from this web site because I plan to use them again.)

This page was last updated on March 22, 2000.