NATS 101 Quiz #1 Study Guide
(click here to download this study guide in Microsoft WORD format)

Questions on Quiz #1 will come from topics on this study guide together with material on the Practice Quiz Study Guide.

Mass, weight, density, and pressure. Mass is the amount of a particular substance. On the earth gravity pulls downward on a mass producing weight. Pressure at any level in the atmosphere is a measure of the weight of the air above (this is one way of thinking about and understanding pressure). Pressure is defined as force divided by area and acts like a force (a force that pushes upward, downward, and sideways). Common pressure units and typical sea level pressure values. What instrument is used to measure air pressure? About when was it invented? Pressure and air density (density = mass divided by volume) both decrease with increasing altitude (you should be able to explain why). What relationship is there between the rate of pressure decrease and air density (i.e. does pressure decrease most rapidly in high or low density air)?

Sample questions (from the Fall 2000 quiz packet)
Practice Quiz: 15, EC2, EC3          Quiz #1: 3, 17           Final Exam: 6, 11

Ideal Gas Law. This is a microscopic-scale explanation of air pressure. Two equations:

P = N k T / V and P = (rho) R T


N is the number of air molecules in a volume V, T is temperature and  rho is density.  R and k are both constants (you can pretty much ignore them). 
You should be able to determine what will happen to the pressure in a rigid container or something flexible like a balloon if you change the variables in the equation above.  What variables could you change together in such a way that the pressure would stay constant?

Ideal gas law applications.  If you heat or cool a parcel of air in the atmosphere, Charles' law says the density (volume) will change in a way that keeps the air pressure inside the parcel constant (the pressure inside the parcel remains the same as the pressure of the air surrounding the parcel). 

Upward and downward forces acting on air parcels (the strength of one of the forces depends on the air inside the parcel, the other on the air outside the parcel). These two forces are usually in balance. What happens to the balance when you warm or cool a parcel of air?  Basically you should be able to explain why a balloon of hot low density air rises and a balloon of cold high density air sinks.

Archimedes Law.  An object immersed in a fluid (a liquid like water or a gas like air) experiences an upward bouyant force that is equal to the weight of the fluid displaced by the object.  Basically objects that are less dense that the fluid around them float, objects that are denser than the fluid surrounding them sink.  What causes the upward bouyant force?

Layers of the atmosphere. Troposphere: lowest layer in the atmosphere, decreasing temperature with increasing altitude (why is the warmest air found near the ground), contains most of the water vapor and clouds, can be unstable (strong vertical air motions possible). Tropopause. Stratosphere: there's an isothermal layer and a temperature inversion layer (what causes air to warm in the stratosphere), stable layer, contains the ozone layer. Approximate altitudes of these layers. Units: meters, kilometers, feet, miles.

Sample questions
Practice Quiz: 8, 16          Quiz #1: 13, 14, 16, 17, EC2          Final Exam: 19, 22

Station model notation. How and where are the following weather variables plotted: cloud cover, temperature, dew point temperature (typical values for Tucson), wind direction and speed, common weather symbols (rain, snow, fog, rain shower, thunderstorm, tropical storm and hurricane), pressure.  Units. After pressure is measured, what important adjustment is made before the pressure is plotted on the surface map? Why is that necessary? Average and typical range of sea-level pressure values.

The following material won't be on Quiz #1
Surface weather maps. A new map is prepared hourly. What time zone or time reference is used? 24-hour clock (what is the local time when it is 17:30 MST in Tucson). Isobars and isotherms. Small horizontal differences in pressure cause the wind to blow. Air motions around high and low pressure centers (northern hemisphere). Strong and weak pressure gradients. Convergence and divergence. Rising and sinking air motions. How do wind motions around highs and low affect the temperature pattern? Cold fronts and warm fronts (where is the warm and cold air, what direction are the fronts moving).

Sample questions
Practice Quiz: (2, 11), 14, 19          Quiz #1: 6, (7, 8, 9), 10, (11)           Final Exam: (7, 10, 34), 52
(we may not have time before Quiz #1 to cover the material needed to answer the questions in parentheses)

Reviews
Mon., Sep. 21
4-5 pm
FCS 225
Tue., Sep. 22
4-5 pm
Haury 129
Wed., Sep. 23
4-5 pm
FCS 225