Final Exam Emphasized Topics Flashcards
(88 cards)
Polar Front Theory
- Stationary Front
- Frontal Wave
- Open Wave
- Mature (initial occlusion)
- Advanced occlusion
- Cutoff cyclone
Rossby waves are:
Long waves
Corriolis force is stronger at ___ making winds faster
Ridges
Wind slows during ___
Wind speeds up during ___
- Convergence
- Divergence
What is the Rossby Redox
- Short waves move faster
- Short waves are embedded in the background of longwaves and are much more active
How do short waves cause storms (cyclones)?
- Begins with stationary polar front and a steady flow above
- As the shortwave moves through the upper air flow, convergence and divergence generate high and low centers
- This starts. the polar front moving, generating a warm front with air moving N and cold front where it moves S
- Storm dissipates when the surface low isolates from the upper air divergence
Barotropic/ Baroclinic
- Temperature contours and isoheights are parallel
- no advection = Wind transported horizontally by the wind
Baroclinic Instability
- Short wave pushes south across temperature contours
- Cold air is transported into region of convergence deepening the trough
- Warm air is brought into region of divergence, strengthening the ridge
Cooling air ___, whereas warm air ___
compresses down
Warm air expands up
Numerical Weather Prediction (NWP)
Considers:
- domain size
- resolution
- initial conditions
- model assumptions
Watch
Atmospheric conditions are favorable for hazardous weather although location and time are uncertain
Warning
Hazardous weather is actually occuring or imminent within the forecast area
What developes a tropical disturbance into a tropical cyclone
- Warm sea surface
- Adequate Coriolis effect: 5 degrees from the equator
- weak vertical wind shear: no strong upper tropospheric flow
- humid air in mid troposphere
What does the saffir simpson scale measures…
Rates tropical storm strength on a scale from 1-5
Easterly Waves
- Travel east to west in the trade winds
- troughs in mid-latitude upper flow - winds slows when entering easterly wave
- Convergence -> wind increases when exiting easterly waves
- Divergence -> low level convergence causes upward motion
Requirements for tropical storm/cyclone formation
- Storm is powered by latent heat release in clouds
- adequate coriolis effect provides rotation
- weak verticle wind sher required allowing deep vertical orginization and development
- Moist mid-troposhere
Hurricanes weaken or die when…
They loose their source of moist air by moving over land, or over colder water
- this reduces the supply of latent het that powers the storm
How does cyclic flow in the lower troposphere, becoming anticyclonic in the upper troposphere
Wind are strongest in the lower troposphere, then decrease in the upper troposphere until they turn and circulate in the opposite direction at the top of the storm
Cyclostrophic Flow
Pressure-gradient + Coriolis effect + friction = V2/R
- At the eye wall of a hurricane
- pressure gradient much larger than friction
- weak Coriolis
- parcels move rapidly in a tight circle
- parcels cannot make ny further inward progress, so winds in the eye are weak
True or False: the eye of the storm is almost cloud free
True
Cyclostrophic Radius
some air descends to replace eye air fed into base of eye wall clouds
What are the pressure trends as the eye approaches
pressure drops as the eye approaches and winds peak near the eye wall
Storm Surges
- strong onshore winds
- shallow sloped shore
- narrowing bay
- high tide
Region of Maximum heating
- Where the solar altitude angle reaches 90 degrees
- varies between the tropic of cancer and the tropic of capricorn