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Material Type: Exam; Class: PHYSICAL METEOROLOGY; Subject: Atmospheric and Oceanic Science; University: University of Maryland; Term: Fall 2008;
Typology: Exams
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AOSC400 Midterm Examination Solution October 29, 2008
This is a 50minute closed book examination consisting of 10 multiple choice questions (~1min each) and one short essay (~10min). Please relax. Then look over the whole examination before beginning.
Part 1 (1pt each)
ANSWER: a
ANSWER: b
ANSWER: b
ANSWER: c
ANSWER: b
ANSWER: b
ANSWER: d
ANSWER: c
ANSWER: a
c. decrease; increase d. decrease; decrease
ANSWER: a
Part 2 (10pts each)
(a) density = 1.19 kg/m (b) Within the container, an increase in pressure must be caused by an increase in temperature. New temperature = 586 K.
Figure 1 : a cloud
This is a photograph of a cumulonimbus cloud. Notice the anvil cloud (upper left) which may extend to 10km altitude or beyond, contains ice crystals, and takes its shape from high level winds blowing to the left in this picture. Note the central column with strong uplift and indication of rain below the lowest cloud level.
surface low pressure?
a) Standard sea level pressure is 1015 mb. Pressure decreases with height approximately exponentially as p(z)=1015*e-(z/8.5km). Plugging in P(z)=750mb gives z=2.5km height. So, 750mb is the pressure we might expect to find in Vail, Colorado for example. Incidentally, the lowest surface pressure associated with a hurricane was Wilma at 882mb. b) Air would still rise at the center of a surface low pressure. Incidentally, the Southern Hemisphere behaves kind of like the Northern Hemisphere, only with reversed rotation (in other words, the Coriolis force is negative).
Two processes describe the growth of rain drops:
Collision and coalescence : Cloud droplets collide with each other. If they stick to each other, or coalesce, the drop grows. The faster the droplet descends the more collisions can be expected. This process is most important in the tropics and when rain drops are already big. For smaller droplets the most important process is:
The Bergeron process depends on the fact that the saturation vapor pressure with respect to ice is less than the saturation vapor pressure with respect to water. Pure water droplets freeze only at temperatures of -40°C. Tor Bergeron realized that as air reaches saturation and a mixture of water and ice exists at the same time then the difference in vapor pressures will cause the water droplets to evaporate and the ice crystals to grow through sublimation.