Notes
http://science.discovery.com/videos/time-doppler-effect.html
Farenheit
Fahrenheit usually refers to a
temperature scale proposed in 1724 by, and named after, the
physicist
Daniel Gabriel Fahrenheit
(1686–1736). Today, the scale has been replaced by the
Celsius scale in most countries; it is still in use for
non-scientific purposes in the
United States and a few other nations, such as
Belize.
On the Fahrenheit scale, the
freezing point of
water is 32 degrees Fahrenheit (°F) and the
boiling point 212 °F (at
standard atmospheric pressure),
Celcius
Celsius (also known as
centigrade) is a
temperature scale that is named after the Swedish astronomer
Anders Celsius (1701–1744), who developed a similar temperature
scale two years before his death.
From 1744 until 1954, 0 °C was defined as the freezing
point of water and 100 °C was defined as the boiling point of water, both at
a pressure of one
standard atmosphere. Although these defining correlations are
commonly taught in schools today, by international agreement the unit
"degree Celsius" and the Celsius scale are currently defined by two
different points:
absolute zero, and the
triple point of
VSMOW (specially
prepared water).
Kelvin
The kelvin (symbol:
K) is a
unit increment of
temperature and is one of the seven
SI base units. The
Kelvin scale is a
thermodynamic (absolute) temperature
scale where
absolute zero, the theoretical absence of
all thermal energy, is zero kelvin (0 K). The Kelvin scale and the kelvin
are named after the British physicist and engineer
William Thomson, 1st Baron
Kelvin (1824–1907), who wrote of the need for an "absolute
thermometric scale".
Problem Concerning the Temperatures at the center and surface of the Sun
The Solar Physics Group at NASA's Marshall Space Flight Center was formed in the early 1970's in conjunction with the Apollo Skylab Mission. Some facts about the Sun published by this group are given below:
C = K - 273.15 F = (9/5)C + 32
| Kelvin | Centigrade | Fahrenheit | |
| Surface Temperature | 5770 | 5496.85 | 9,926.33 |
| Central Temperature | 15,600,000 | 15,599,726.85 | 28,079,540.34 |
2. What are these estimates based on? How are they determined?
3. Explain a rationale for the center being hotter than the surface.
The solar interior is separated into four regions by the different processes that occur there. Energy is generated in the core, the innermost 25%. This energy diffuses outward by radiation (mostly gamma-rays and x-rays) through the radiative zone and by convective fluid flows (boiling motion) through the convection zone, the outermost 30%.
Surface exposed to low temperature of space