Geography-Exam-#1 Flashcards
What happens as you go higher into the atmosphere?
Density Decreases
Air Pressure Decreases
Temp. Decreases.
Lapse Rate
Go higher in the troposphere = temp. decreases.
Electromagnetic Radiation (EMR)
Energy that travels in wave form at the speed of light.
Insolation
- EMR that arrives at Earth’s atmosphere or surface.
- Drives most Earth processes!
How does wavelength relate to amount of energy?
- Shorter the wavelength = Higher energy
- Longer the wavelength = Lower energy
Ionosphere
-Absorbs gamma rays, X-rays, and Shorter UV rays
Ozonosphere (Ozone Layer)
-Blocks ultra violet-c and UV-B
Energy Budget
- Daily energy patterns are like a budget.
- Depend on day length and sun angle.
- Summer = more energy in-less energy out; spring/fall = equal energy in & out; winter = less energy in-more energy out.
What are the three reasons for the season?
- ) Revolution (around the sun).
- length of season
- ) Rotation (Earth’s spin)
- Day/Night length
- ) Tilt of Earth (23.5 degrees)
- changes over time
- MOST IMPORTANT - Wouldn’t have seasons at all without the tilt.
Reflection
Bouncing of radiation off of a surface
Albedo
- Percentage of insolation that is reflected
- Earth’s albedo = 31%
-IMPORTANT: If it changes, climate will change!
Absorption
Assimilation of radiation by matter
-69% not reflected by Earth is absorbed.
Emission
Loss of assimilated radiation back into space
-If this didn’t occur, it would get too hot!
Conduction
Molecule to molecule heat transfer
-Sit on a cold metal chair, the heat from your body will heat up the chair.
Convection
Energy transfer through liquids and gasses by mixing.
- Air condition blows out cool air (more dense) that sinks and the warm air rises and is drawn in by the AC.
- Convection current is set up, room cools.
Latent Heat
Energy used in a phase change of matter with no change in temp.
-When we sweat. Our body’s get hot and then we start sweating so our bodies cool down.
Sensible Heat
Energy used to change the temp. of matter.
-Can be felt & measured
-The warmth you can feel from the sun or a campfire
Weather
Short-term day to day condition of the atmosphere.
Meteorology
scientific study of the processes of the atmosphere
Climate
The long-term average (decades) of weather conditions
Measuring Temp.
1.) Fahrenheit —- F -> Celsius (F-32)*(5/9)
- ) Celsius Freezing = 0 degrees Boiling = 100 degrees
- C -> F = (C*1.8) + 32
- ) Kelvin Scale - Absolute zero
- (-273) degrees Celsius - (-459) degrees F
- C -> K = C + 273.15
5 Factors that control temperature
- ) Albedo
- )Latitude
- )Altitude/elevation
- )Maritime or continental location
- ) Cloud cover
1.) Albedo
- Dark surfaces = absorb more electromagnetic radiation
- Light surfaces = reflect more EMR
2.) Latitude
- Insolation = different at different latitudes
- Strongest at equator - weakens as you go N or S
- Curve of the earth & Day length
- Insolation intensity drops when u move away from sub-polar point.
- From equator to poles = Earth goes from continually warm, to seasonally variable, to continually cold.
- Strongest at equator - weakens as you go N or S
3.) Altitude/Elevation
Lapse rate- go higher in troposphere = temp. decreases.
-Mimics latitude effect - higher latitude = colder
4.) Maritime or Continental Location
Maritime = Near water Continental = away from water
- water and land heat differently
- Land (more extreme temp. occurs) = warms and cools rapidly = less evaporation (lower latent heat)
- Water (produce moderate temp. patterens) = warms and cools slowly = more evaporation (more latent heat)
-Gulf stream (65 N) = mean temp above freezing - milder temps due to warm water
5.) Cloud Cover
- Block insolation (Cooling effect) = Day
- Trap emitted radiation (warming effect) = Night
Which pole is colder? North or South?
South Pole (Antarctica) - landmass surrounded by ocean + higher elevation
Greenland = cool in summer due to altitude
Earth’s Energy Balance is equal or unequal?
- Unequal
- Drives atmosphere and ocean circulation
- Lots of energy at equator, low energy at N & S pole