Transcript Day-19
Astronomy 1010-H
Planetary Astronomy
Fall_2015
Day-19
Course Announcements
•
How is the sunset/sunrise observing going?
•
Dark Sky nights – Wed. 10/7 starting at 7:30pm – at the
Observatory.
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Exam-2 will be Friday, Oct. 9; Ch. 3, 4, & 5
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SW-chapter 5 posted: due Fri. Oct. 9
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No lab next week – Fall Break
Emitted Light
Luminosity: amount of light leaving a
source.
The amount and type of light leaving a
source changes as an object heats up or
cools down.
The hotter an object is, the more luminous
it is.
The hotter an object is, the bluer it is.
Dense objects emit
a blackbody (or
Planck) spectrum.
Continuous.
Gives light at all
wavelengths.
Example:
incandescent light
bulb.
For two objects of
the same size, the
hotter one will:
• Emit more total light
at all wavelengths.
• Emit more total
energy every
second.
• Emit light at shorter
wavelengths, on
average.
Stefan’s Law
Flux is the total amount of energy emitted
per square meter every second (the
luminosity per area).
Then:
F T
4
where T is the temperature, F is the flux,
and (sigma) is called the StefanBoltzmann constant.
Hotter objects emit much more energy (per
square meter per second) than cool objects.
Wien’s Law
The peak wavelength of a blackbody is
inversely proportional to its temperature.
2
,
900
,
000
nm
K
peak
T
Peak wavelength peak : the wavelength of
light of a blackbody that is emitted the
most.
Here the wavelength is in nanometers and
the temperature is in kelvin.
“Hotter means bluer.”
L
B
2
4r
Brightness is the
amount of light
arriving at a
particular place.
Decreases as the
distance from a light
source increases,
obeying an inverse
square law.
The light spreads
out over a greater
area.
Temperature is a measure of the average
speed of the motions of atoms.
Kelvin scale: Water freezes/boils at 273 K /
373 K.
Absolute zero is when thermal motion stops.
Equilibrium Temperature
Balance between absorbed and radiated energy.
Albedo (reflectance) of a planet.
a = 1: 100% reflection
a = 0 : 100% absorption
Energy absorbed = R2 * L/4d2 * (1 – a)
Energy Radiated = 4R2 * T4
Radiation laws help figure out the equilibrium
temperatures of the planets.
Distant planets are cold mainly because of
the inverse square law of light.
Balance of heating and cooling.
CONNECTIONS 5.1
A stable equilibrium is a balance that is unlikely to
change, while an unstable equilibrium can easily
be nudged away from its balance point.
Static equilibrium involves a situation where
forces are balanced and opposing each other, so
nothing changes.
Dynamic equilibrium involves a situation that is
always changing, but remains in balance.
MATH TOOLS 5.3
With the Stefan-Boltzmann law, you can find
Earth’s flux using its average temperature of
288 K.
Using Wien’s law, you can find the Sun’s
surface temperature using the fact that its
peak wavelength is around 500 nm.
MATH TOOLS 5.4
The equilibrium temperature of a planet
depends on the energy it receives and its
albedo (a), its reflectivity.
MATH TOOLS 5.4
The equilibrium temperature of a planet
depends on the energy it receives and its
albedo (a), its reflectivity.
Simplifying:
PROCESS OF SCIENCE
Confirmation of an idea from different
fields of science can be a strong indication
of the truth of that idea.
Exam-2 To Here!
Telescopes & Instruments
The telescope is the
astronomer’s most
important tool.
Purpose: to gather
light of all kinds.
Two kinds of optical
telescopes:
reflecting and
refracting.
Invented in 1608 by
Hans Lippershey.
Telescopes come in three
general types
Reflectors use mirrors to reflect
the light to a focus
Refractors use lenses to bend
the light to a focus
Catadioptric telescopes use both lenses and
mirrors
Telescopes
Telescopes have three functions:
1.
Gather light
2.
Resolve objects
3.
LGP ∝ Area = πR2
Θ = 2.06 X 105 (λ/D)
Magnify EXTENDED objects
The most important property of any
telescope is to gather large amounts
of light and concentrate it to a focus.
Light Gathering Power Area radius 2
Refraction is the bending of
light when it goes from one
medium to another
“n” is the
index of
refraction.
c
n
v
Refraction is
governed by
Snell’s Law:
n1 sin 1 n2 sin 2
If we curve the surface and
make a lens, we can get the
light to concentrate to a point
Refracting telescopes
use lenses.
Objective lens: refracts
the light.
Aperture: size of the
objective lens (larger
aperture gathers more
light).
The objective lens is
placed in the aperture.