AOS 3 Final Flashcards
What does planetary scale circulation mostly result from?
1) The difference of temperature between the equator and the poles (PGF)
2) The rotation of the planet (Coriolis)
3) Distributions of land and water over the planet (friction)
Describe the polar front
Cold air from the pole meets warmer air from the subtropical high at the polar front
Upper winds are well-predicted within the ________ but completely off for the _________
Hadley cell, Ferrel cell
In which direction does the air in the polar jet stream
flow in the Northern Hemisphere?
From west to east
Compare the polar jet stream and subtropical jet stream.
- Polar jet is very strong (110 mph in the winter) & effects US weather development
- Subtropical jet is much weaker & brings warm moist air to the US
Describe rossby waves
- The largest of the atmospheric long waves
- three to seven Rossby waves circle the globe at any one time, and each has its own wavelength and amplitude
- Although they have preferred anchoring positions they do migrate eastward (very slowly)
What happens when rossby waves “break”?
- seen as oscillations in the polar jet stream
- By moving the jet stream around, they can affect the weather
- “Breaking” Rossby waves can be considered a source of low and high pressure centers
What happens to ice crystals in the Bergeron process
Ice crystals grow rapidly at the expense of supercooled droplets (via net deposition and net evaporation)
Describe the process of precipitation.
- Unsaturated air rises and cools by adiabatic expansion, reaching saturation
- Presence of CCN allows for condensation, leading to formation of tiny droplets
- Droplets grow by additional condensation
For it to rain, droplets need to fall ________ than the vertical velocity in the updraft
faster
Describe the terminal velocity state of equilibrium
drag force equals gravitational force
Describe Collision Coalescence
- Warm clouds grow
- cloud droplets collide and stick together
- Promoted by large collector drops, which have high terminal velocities so they fall faster and collide with smaller drops
What is riming?
liquid water freezes onto ice crystals
What is aggregation?
ice crystals collide and merge via thin coating of liquid water (ice crystals come together to form snowflakes)
What limits the growth of ice particles by the Bergeron process?
- amount of supercooled water in the cloud
- time an ice particle remains in the cloud
Describe snow crystals.
- single crystals
- depend on temperature and degree of supersaturation (for ice)
Describe snowflakes. How do they differ for warm/cold clouds?
- aggregates of snow crystals
- mostly formed by riming in warmer clouds and form dense wet snowpack (snowballs)
- formed by aggregation in colder clouds making less desne powdery snowpack (skiing)
What is lake effect snow?
- Develop as the warm lake waters evaporate into cold air
- Friction over land reduces winds and creates a lifting mechanism downwind from the lake
Compare rain in warm and cool clouds.
- Cool clouds:
Most middle-latitude precipitation starts out as snow, then melts to rain - Warm clouds:
Predominant in the tropics, starts and falls as rain
Compare graupel and hail
Graupel: Rimed ice crystal
Hail: Concentric layers of ice built around graupel (wet growth results in solid ice)
Both results from in-cloud processes!
What are possible types of precipitation that could originate from a cold cloud?
- Rain
- Snow
- Hail
- Graupel
- Freezing rain
- Sleet
Compare the different spatial scales
Global Scale
- planetary waves
- hadley cell
Synoptic scale
- extratropical cyclones
- weather systems
Mesoscale
- thunderstorms
- tornadoes
(smaller length and time scales as you move down)
Describe the single-cell model
- Simplified model of the general circulation proposed by Hadley (1735)
- Based on idealized water planet with no effects of rotation (no CF, no friction)
- Deflection by Coriolis
- One single cell in each hemisphere
- First model of a thermally driven circulation
Describe the three-cell model
- Improved model of the general circulation proposed by Ferrel (1865)
- Each hemisphere divided into three cells
- Not perfect, but more realistic thansingle-cell model