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Instructions for Side by Side Printing
  1. Print the notecards
  2. Fold each page in half along the solid vertical line
  3. Cut out the notecards by cutting along each horizontal dotted line
  4. Optional: Glue, tape or staple the ends of each notecard together
  1. Verify Front of pages is selected for Viewing and print the front of the notecards
  2. Select Back of pages for Viewing and print the back of the notecards
    NOTE: Since the back of the pages are printed in reverse order (last page is printed first), keep the pages in the same order as they were after Step 1. Also, be sure to feed the pages in the same direction as you did in Step 1.
  3. Cut out the notecards by cutting along each horizontal and vertical dotted line
To print: Ctrl+PPrint as a list

19 notecards = 5 pages (4 cards per page)

Viewing:

Pressure, weather maps, energy

front 1

The 3 primary roles of Ozone (O3)

back 1

  • absorbing UV radiation
  • absorbing Earth's longwave radiation
  • being a surface pollutant

front 2

Where Ozone most concentrated

back 2

The stratosphere

front 3

The 3 most degrading compounds for the ozone layer

back 3

CFCs, nitrous oxide, bromine compounds

front 4

What winds and stability control the rate of

back 4

the rate of mixing pollutants with clean air

front 5

What atmospheric aerosols are

back 5

solids or liquids suspended in the air

front 6

What primary aerosols are

back 6

aerosols emitted directly into the atmosphere

front 7

The 2 probable sources of Earth's, Mars', and Venus' primitive atmosphere

back 7

outgassing and comets and asteroids

front 8

What our was likely most of our primitive atmosphere

back 8

Water vapour and CO2

front 9

Processes that contributed to our current atmosphere

back 9

Atmospheric thinning and photosynthesis

front 10

The hypothesis that proposes the Earth-Atmosphere systems are self-regulating and work to maintain ideal conditions for life to continue

back 10

The Gaia hypothesis

front 11

The other name for Boyle's Law

back 11

Constant temperature

front 12

The other name for Charles's Law

back 12

Constant pressure

front 13

The two gas laws with directly proportional variable and temperature on the x-axis

back 13

Charles's Law (constant pressure) and constant volume

front 14

The relationship between the pressure of a gas, with constant temperature, if you increase its volume

back 14

Inversely proportional

front 15

Define an ideal gas.

back 15

a gas which has no attractive forces between molecules

front 16

The variable that replaces volume in the ideal gas equation in atmospheric sciences

back 16

density

front 17

the temperature that dry air would need to be in order to have the same density as the actual air

back 17

Virtual temperature (Tv)

front 18

A summary of the 2 properties of ideal gasses

back 18

Air is compressible and warm air is less dense than cold air

front 19

The height above the surface at which warm air will have more pressure than cold air

back 19

Any height