Test 2 Review Flashcards
General, worldwide atmospheric circulation (ex. trade winds, westerlies, polar easterlies)
Primary circulation
What are the three levels of atmospheric circulation?
Primary, secondary, and tertiary
Migration of high and low pressure systems; mesoscale wind circulation between high and low pressure systems
Secondary circulation
Local winds (ex. Santa Ana winds, land breeze, sea breeze)
Tertiary circulation
The force exerted on you by air molecules; although air molecules are invisible, they still have weight and take up space
Air pressure
A tube closed at the top, containing mercury with a Toricelllian vacuum above it and a mercury bath at the open bottom end; the pressure on the open bath determines the height of the mercury column above it
Mercury Barometer
A closed, flexible container of gas and attached to the container is a mechanism to move a pointer on a scale; when atmospheric pressure changes, the container changes internal volume, moving the scale to indicate the pressure outside of it relative to the fixed pressure inside it
Aneroid barometer
What is the normal sea level air pressure?
14.7 lbs/in2 or 1013.2 mb
The force which results when there is a difference in pressure across a surface (control on wind velocity)
Pressure gradient force
True or False: the greater the pressure gradient, the faster the wind flow
True
How is wind generated?
- Air rises at point B because it is warmer and a void is created
- Low pressure at point B
- Air pressure at point A is higher
- Air moves from point A to point B
- Surface wind is created
A breeze blowing toward the sea, especially at night, owing to the relative warmth of the sea
Land breeze
A breeze blowing toward the land from the sea, especially during the day, owing to the relative warmth of the land
Sea breeze
Since the earth rotates on its axis, it produces a deflective force that affects wind direction (if the earth did not spin on its axis, winds would follow the direction of the pressure gradient); stronger towards the poles; deflected right in the NH and left in the SH
Coriolis force
Acts on the wind flow and the effect becomes more and more severe as you get closer to the surface
Friction force
The part of the atmosphere that lies above the frictional force, on average at an altitude of about 1000m
Free atmosphere
True or False: Coriolis force balances pressure gradient force
True
The theoretical wind that would result from an exact balance between the Coriolis effect and the pressure gradient force
Geostrophic wind
When the wind swirls clockwise in the northern hemisphere or counterclockwise in the southern hemisphere
Anticyclonic air flow
When the wind swirls counterclockwise in the northern hemisphere or clockwise in the southern hemisphere
Cyclonic air flow
Air comes together at the center of the low near the ground; converging air rises and the water vapor within cools and eventually condenses
Air convergence
Air moves away from the center of the high near the ground; air has to come from above to fill the void, leads to a sinking motion in the center of a high pressure system and clear air
Air divergence
True or False: Air convergence is associated with high pressure
False: Air convergence is associated with low pressure and air divergence is associated with high pressure
Wind blowing steadily toward the equator from the northeast in the northern hemisphere or the southeast in the southern hemisphere, especially at sea
Trade winds
A wind blowing from the west; the belt of prevailing winds in the mid-latitudes of the northern and southern hemispheres; generated from the subtropical high pressure cell
Westerlies
Why do the Westerlies gather strength and speed in the southern hemisphere?
Because there is less land there to cause friction to slow them down, an almost unbroken belt of oceans
Known to sailors as doldrums, the area encircling the earth near the equator where the northeast and southeast trade winds come together
Intertropical Convergence Zone
What months do the dry monsoon occur in?
October through May
Picks up moisture from the ocean and brings the rain that sustains agriculture
Wet monsoon
A tropical atmospheric circulation that is defined by the average over longitude, which features rising motion near the equator, poleward flow 10-15 km above the surface, descending motion in the subtropics, and equator-ward flow near the surface
Hadley Cell
The average motion of air in the mid-latitudes; characterized by sinking air near 30 degrees and rising air farther poleward
Ferrel Cell
What is the leading edge of the polar easterlies?
The polar front
Boundary between continental polar air mass and topical maritime airmass where frontal precipitations can take place
Polar front
A change in the velocity and trajectory of upper air wind flows
Index cycle
Maintains air masses within their boundaries
Zonal flow
Allows very cold air from the arctic to move to lower latitudes from the tropics
Meridional flow
What is the driving force of ocean currents?
The frictional drag of the winds
Large body of air whose physical properties are more or less uniform horizontally for hundreds of km; horizontal dimension can be as big as a continent and vertical dimension can extend throughout the troposphere
Air mass
What are the air mass classifications?
Maritime, continental, arctic, antarctic, tropical, or equatorial
What are the principal air masses?
- Continental polar in the NH
- Maritime polar over northern oceans
- Maritime tropical in the Atlantic and Pacific
Created because of thermodynamic and dynamic changes
Secondary air masses
Cold air mass moving south over warm land
Thermodynamic
Air mass has to go over topographic barrier
Dynamic
What is developing when continental polar and maritime tropical air masses clash and the maritime tropical air mass at the surface is forced to rise above the ground
Mid-latitude cyclone
What are the stages of a mid-latitude cyclone?
- Frontogenesis and cyclogenesis (early stage)
- Mature (open) stage
- Occluded (dying) stage
Which stage: creation of fronts, warm/moist air rises, condensation reached, low pressure forms at apex of two fronts
Frontogenesis
Which stage: creation of a mid-latitude cyclone, warm air is the fuel tank, not producing frontal precipitations, stratiform and cumuliform clouds
Cyclogenesis
Which stage: storm is fully developed and precipitation is generated, but it has not reached full potential, cold front travels faster than the warm front and cold air is actively pushing warm air up
Mature (open) stage
Which stage: cold front catches up with the warm front and no warm sector is connected to the storm, most intense phase in terms of heavy and steady rainfall and strong winds
Occulded (dying) stage
Which front is typical of zonal flow conditions
Stationary front
Upper air flow starting to slow down and move above ground, enters a meridional phase
Frontal wave
Warm air glides on top of cool air
Warm front
Cold air is actively pushing warmer air aloft
Cold front
300 yards diameter, winds more than 300 mph, traveling speed 25-40 mph
Tornado
When is tornado season?
April-July, 74% take place March-July
Why does tornado season start in April?
In April, the polar jet stream, polar front, and continental polar air mass are slowly retreating to higher latitudes. Clashes between warm/moist and cold air masses along the polar front are more severe.