This site is 100% ad supported. Please add an exception to adblock for this site.

Physical Geography

Terms

undefined, object
copy deck
Mesospause
Coldest portion of Atmosphere
Hydrostatic Balance
relationship between gravity and air pressure
Altostratus
mid level blanket, sun just visible, gray day
Radiant Energy
Transferred in streaming waves
radiation fog
ground cools faster than air
Relative humidity
ACTUAL amount of water vapor divided by the CAPACITY of the air
Troposphere
90% mass of the atmosphere
Cloud Formation
Requires condensation nuclei
Wein's Law
HOT objects have a shorter wavelength than COLD objects
Transmission
Passage of shortwave and long wave energy through the atmosphere or water
stratocumulus
soft gray, globby, irregular overcast
Stratosphere
9% mass of atmosphere
Perihilion
period when the earth is closest to sun
Absolute humidity
Mass of water vapor (grams) per volume of air (cubic meters)
Where does Geostrophic Wind Occur?
Only occurs above surface (~1.5 miles) due to friction
Freezing rain
snow melts completely and freezes after it hits the ground
Bergeron Process
Ice crystals grow at the expense of water droplets
advection fog (ocean, snow)
warm air over cold surface
Sleet
partially melted snow that refreezes before it hits the ground
1st law of thermodynamics
Energy is neither created nor destroyed
Three Components of wind
PGF, Coriolis, Friction
Stratosphere
Temperature INCREASES with height
Dew point
Temperature to which air must cool for condensation to occur (saturation)
nimbostratus
drizzle, rain clouds
Virga
Rain that doesn't hit the ground
Kirchoffs Law
All objects emit radiation and absorb radiation
Cirrus
Wispy, Feathery, Delicate
Cirrostratus
High thin veil, ice crystals, halos
Specific humidity
Mass (grams) of water vapor per total mass of air (kilograms)
PGF
Difference in pressure over distance
Scattering
Radiation comes in contact with molecules, which redirect the light's movement
Aphelion
period when the earth is furthest from the sun
PGF
Starts atmospheric motion, Determines wind speed
Temperature Inversions
Layer where lapse rate is much less
Troposphere
Heat Source is Ground
Advection
Horizontal Transfer important in Liquid and Gases
Coriolis
deflection of wind at the earth's surface to the right
Vertically Developed Clouds
Cumulus, Cumulonimbus
Land Sea Breeze
due to thermal differences, reverses diurnally
Cumulus
Puffy, Flat based, Fair weather
Hail
Particles of ice held aloft by thunderstorm updraft
radiation fog
most common type of fog
Monsoon
seasonal reversal of winds
Formula for Pressure
R (Density) (Temperature)
Mountain/Valley Winds
refers to the sinking cool air at night into the valley
Low Clouds
stratus, stratocumulus, nimbostratus
Collision-Coalescence: tropics (warm)
Particles bump into each other and merge together
Isobars
Lines of equal pressure
radiation fog
fog that occurs on clear calm nights
Convection
Vertical Transfer important in Liquid and Gases
Geostrophic wind
Perfect Balance between Coriolis effect and PGF
High Clouds
Cirrus, Cirrostratus, Cirrocumulus
Sensible Heat
Heat energy 'sensed' by thermometers
Middle Clouds
Altostratus, Altocumulus
stratus
uniform, featureless, high fog
Albedo
Percent of energy reflected by a surface
Troposphere
Zone of weather
Thermosphere
Only part of atmosphere being heated by the sun
advection fog (sea smoke, hot tubs)
cold over warm moist surface
Cumulonimbus
thunderclouds, well developed, anvil top
Cirrocumulus
dappled, mackeral sky
Valley fog
Cold air moving into a valley causing condensation
Factors Affecting Insolation at Surface
Sun Angle, Day Length, Absorption, Reflection, Scattering
Specific Heat
The amount of energy required to raise 1 gram of substance 1° Celsius
4 Spheres of Geography
Atmosphere, Hydrosphere, Lithosphere, Biosphere
Latent Heat
amount of energy absorbed or released during phase changes of water
Mountain (Chinook, Santa Anna)
warm dry air on the down slope of the leeward side of the mountains
Stefan-Boltzmann Law
HOT objects emit more radiation than COLD objects
Types of Energy
Kinetic, Potential, Radiant
Stratosphere
Warming is due to ozone
Altocumulus
cotton balls
Density Formula
mass/volume

Deck Info

72

permalink