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96 Cards in this Set

  • Front
  • Back
power
-rate of energy transfer
-measured in watts (= joules)
matter
-emit
-absorb
-transmit
-reflect/scatter
light
-electromagnetic wave
-pieces: photons
-wL, Fr, energy
forms of light
-XR
-UV
-IR
-Radiowaves
-Microwaves
-Visible
-Gamma Rays
matter
-atoms (pro+, neutron (neutral), elec-)
-isotope (diff. # of neutrons)
-molecule (2+ atoms)
isotope
-same amount of protons
-dif amount of neutrons
phases
-liq, gas, solid, plasma
-g straight to s - sublimation
-dissociation
dissociation
-high temps
-ionization: strips electrons
-turns into a plasma
energy levels
-cannot start in an excited state
-only certain energy levels
-one or the other, no in btw
continuous spectrum
-rainbow
-thermal radiation: can find temp
-nothing blocking the light
absorption spectrum
colors, missing black spaces
-colors are missing
-more colors

-cool cloud btw light source
emission spectrum
-black background
-colors against it
-more black
doppler effect
-how fast something is moving towards/away
-shorter wL: blueshift (Toward)
-longer wL: redshift (Away)
telescope parts
-focus/focal plane
-light collecting area = Ang. Res. (separation of objects)
refracting telescope v. reflecting telescope
-Bending/Lens
-Reflectin/Mirror
uses of a telescope
-imaging
-spectroscopy (object's spectra)
-time monitoring (how brightness changes with time)
ground restrictions of a telescope
-light pollution
-turbulence (twinkling)
-adaptive optics overcame this but they work better in space
interferometry
multiple telescopes working together to get better detail/ang res
clues to SS formation
-rot/orbit organization
-2 groups of planets
-huge # of com/ast
-exceptions to patterns
nebular theory
-solar nebula cloud collapsed into itself
-orderly patterns
-flatter, hotter, faster disc
2 types
-planetismals: accretion
-beyond the frost line: where ices can condense
-rocks/metals
-ices: hy compounds, gases
asteroids/comets
-leftovers
-heavy bombardment: when most craters formed
-collisions/craters
-Oort Cloud, Kuiper belt
-asteroid belt
exceptions
-collisions
-close encounters with planetismals
-giant impact (material from mantle): moon
age of ss
-radiometric dating
-decay, half life
-4.5 by
atmosphere
-layer of gas that surrounds
-creates pressure
-absorb/scatter sunlight
-create wind/weather
-w/ solar wind: magnetosphere
-GHE
Greenhouse effect
-GH gases absorb visible light
-reemit infrared
-the gases make slow their escape
-creates heat
-heats up planet
-would be below freezing w/o it
earth's atm
1. troposphere (GH gas warming)
2. Stratosphere (ozone absorbs UV - only on E)
3. Thermosphere (solar X rays absorbed)
4. Exosphere (lower density, thins out)
weather/climate
-daily/average
-wind patterns - created by atm warming and coriolis effect (rotation)
-convection in Trop = clouds/precipitation
factors of long term change
-axis tilt
-solar brightening
-reflectivity
-GH gas changes
losing gas
-condensation
-chem reactions
-stripped by solar wind
-thermal escape
gaining gas
-outgassing
-evaporation
-sublimation
-surface ejection
Mercury/Moon atm
-thin exos
-surface ejection
-impacts/craters
-some vol/tec
-little activity
Mars
-cold/dry
-low pressure
-frozen water
-co2 conden/sub - winds/dust storms
-changed bc: Loss of gas
-basically dead: small size
-olympus mons: shield volcano
-mostly co2
Venus
-thick co2 atm: run. GHE
-runaway GHE: hot
-no axis tilt/slow rot - no wind/weather/seasons
Earth
-oceans and rocks deal with co2
-stable climate: co2 cycle
-human activity: glob warming
watts
watts x seconds
green grass
reflects green
97 megahertz
el move up/down 97 mil/sec
why is light an ele.mag. wave?
passage of light causes chemical particles to move up/down
x rays
faster
-radio waves: slower
doubly ionized
+2 charge, 6 el = 8 total
electrons do not
orbit the nucleus like planets
does not produce a good thermal spectrum
hot/thin gas
thermal radiation
-hot objects emit more radiation per unit than cool ones
-shape depends on temp
red star
cooler than sun
neptune's spectra
missing red (blue color)
a spectrum cannot find
radius
rotating faster
wider spectral lines
difference btw energy and power
power - rate of of energy
-energy - unit of energy / unit of time
visible light can be spread by a prism or a
diffraction grating
frequency and speed of light can find
wL and energy
shortest to longest wL
-Gamma
-X
-UV
-Visible
-IR
-Radio
light lower than what we can see
-infrared
-radio
opaque to UV
absorbs and reflects
difference btw elements
protons (isotopes: neutrons) (ion - less electrons than p)
atomic mass #

#
13 - add both

6 - protons
4 protons, make it neutral
4 electrons - cancel out
fewer electrons than protons
ion
to find chem comp
wL
where you get a clear image
focal plane
detector
retina
diffraction limit
best ang res without complications
adaptive optics
reduces blurring (turbulence: twinkling)
-Keck I
on ground visibility
-visible, radio, limited UV/IR
interferometry
-multiple tels working together
-better ang res
distortion/color
air scattering affects the path of light
to record a faint image
-lots of pixels
-long exposure
not a major com/ast
all orbit in the same place
not a dif btw ast/com
comets do not just float, they also orbit
e = mc 2 and the sun
explains why mass is burned off by energy (loss of mass)
not true of Eris
it is not a new class of object
why pluto is more like a comet
mostly ice/rock
skimming mars' atmosphere
saves money bc rockets aren't needed
not true of pluto
not largest mass to be called a dwarf planet
disc: hotter/smaller
conser. of energy
disc: faster/smaller
conser. of ang mom
disc shape
collisions of particles
the solar wind
-combines with particles - aurora bor.
-strips away gas
-not stronger today
earth's water
brought by ice planetismals
jovian moons
-backwards orbit
-steep plane (not many comets/ast)
-so many moons: condensation/accretion in the gas disks while forming
why terr planets are more dense
formed in the center of the disc: more dense
-not many ast/com bc they are so dense: hardly any leftovers

-origin of materials: stars that lived/died before
HALF LIFE
every half life: decay DOUBLES
lithosphere
-if it was thicker: no liq water/hotter sur temp
-thin
-btw mantle and crust
cont crust less dense than sea floor
eruption material from subduction
-sea crust: thinner, denser, younger
plate tectonics factors
-mantle convection
-thin litho
heat processes
-accretion
-convection
-thermal radiation
convection
-warm "air" rising and expanding
-cool falling and contracting
magnetic field
-metal core
-rapid rotation
-charged/magnetized particles are affected
subduction zone
seafloor goes under continental crust
what happened to water on venus?
h2o molecules split and hydrogen escaped
-Deuterium
why do we have a stratosphere?
photosynthetic life
co2
-cycle, balances temp: builds in the atm and more GHE happens
-stuck in rocks
-tectonics
-liq water
bar
unit of pressure, standard: earth's sea level
magnetosphere
around planet where charged particles can be trapped
circulation cells
-keep the poles cold
-balances climate
why is mars red?
chem reactions from rock/oxygen