Save
Busy. Please wait.
Log in with Clever
or

show password
Forgot Password?

Don't have an account?  Sign up 
Sign up using Clever
or

Username is available taken
show password


Make sure to remember your password. If you forget it there is no way for StudyStack to send you a reset link. You would need to create a new account.
Your email address is only used to allow you to reset your password. See our Privacy Policy and Terms of Service.


Already a StudyStack user? Log In

Reset Password
Enter the associated with your account, and we'll email you a link to reset your password.
focusNode
Didn't know it?
click below
 
Knew it?
click below
Don't Know
Remaining cards (0)
Know
0:00
Embed Code - If you would like this activity on your web page, copy the script below and paste it into your web page.

  Normal Size     Small Size show me how

Exam #2

CHAPTER 11, 7-SEC.1 &6

TermDefinition
gravitational equilibrium energy supplied by fusion maintains the pressure that balances the inward crush of gravity
energy balance the rate at which energy radiated from the surface of the sun must be the same as the rate at which it is released by fusion in the core
gravitational contraction: the process in which gravity causes an object to contract, thereby converting gravitational potential energy into thermal energy provided the energy that heated the core as the sun was forming, contraction stopped when fusion began
Sun radius + compared to earths 6.9 x 108 m (109 times the earth)
Sun mass + compared to earths 2 x 1030 kg (300,000 time Earth’s)
Sun luminosity 3.8 x 1026 watts
solar wind a flow of charged particles from the surface of the sun  corona: outermost layer of solar atmosphere (1 mill k)
chromosphere middle layer of solar atmosphere
photosphere visible surface of Sun
convection zone energy transported upward by rising hot gas
radiation zone energy transported upwards by photons
core energy is generated by nuclear fusion
fission big nucleus splits into smaller pieces
fusion small nuclei stick together, making a bigger one (SUN and Stars)
solar thermostat the regulation of the Sun’s core temperature that comes when the sun is in both energy balance, and gravitational equilibrium
core temp with fusion rate dropping and rising decline in core temperature causes fusion rate to drop, so core contracts and heats up o rise in core temperature causes fusion rate to rise, so core expands and cool down
solar neutrino problem the disagreement between the predicted and observed neutrinos coming from the sun o early searches failed to find the predicted number o more recent observations find the right number neutrinos but some have changed form
sunspots blotches on the sun that appear darker than surrounding regions o are cooler than other parts of the Sun’s surface (4000 K) o are regions with strong magnetic fields
solar flares huge and sudden release of energy on the solar surface, probably caused when energy stored in magnetic fields is suddenly released. o caused by magnetic activity o send bursts of X rays and charged particles into space
coronal mass ejections bursts of energetic charged particles from the sun’s corona out through the solar system
A planet’s distance from the Sun determines the total amount of incoming sunlight
Rotation and temperature Rotation rate affects the temperature differences between day and night
Reflectivity (albedo) fraction of incoming sunlight it reflects. Low albedo planets absorb more sunlight, leading to hotter temperatures
Venus and earth w/o greenhouse effect Venus would be 510 degrees Celsius colder without the greenhouse effect ○ Earth would be 31 degrees Celsius colder
If Earth were more reflective the temperature would go down
If Earth did not have an atmosphere, the temperature would go down more than 10 degrees Celsius
Ionization removal of an electron
Dissociation destruction of a molecule
Scattering change in photon’s directio
Absorption photon’s energy is absorbed
blue light or red light scatter more Molecules tend to scatter blue light more than red
Molecules can absorb infrared light
Troposphere lowest layer of Earth’s atmosphere ○ Temperature drops with altitude ○ Warmed by infrared light from surface and convection
Created by: katelyn27
Popular Physical Science sets

 

 



Voices

Use these flashcards to help memorize information. Look at the large card and try to recall what is on the other side. Then click the card to flip it. If you knew the answer, click the green Know box. Otherwise, click the red Don't know box.

When you've placed seven or more cards in the Don't know box, click "retry" to try those cards again.

If you've accidentally put the card in the wrong box, just click on the card to take it out of the box.

You can also use your keyboard to move the cards as follows:

If you are logged in to your account, this website will remember which cards you know and don't know so that they are in the same box the next time you log in.

When you need a break, try one of the other activities listed below the flashcards like Matching, Snowman, or Hungry Bug. Although it may feel like you're playing a game, your brain is still making more connections with the information to help you out.

To see how well you know the information, try the Quiz or Test activity.

Pass complete!
"Know" box contains:
Time elapsed:
Retries:
restart all cards