Test 2 Review Flashcards
(142 cards)
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