ch07_rev - Jon Ahlquist 10/5/2006 Chapter 7 Review:...

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Jon Ahlquist 10/5/2006 MET1010 Intro to the Atmosphere 1 Chapter 7 Review: Precipitation ± How do the sizes of a condensation nucleus, a cloud droplet, and a rain droplet compare? ± How does the volume of a raindrop compare to the volume of a cloud droplet? ± Why does water evaporate more easily from a curved surface than a flat surface? ± Why is a wettable condensation nucleus more effective than an unwettable nucleus? ± What is the “solute effect” as it applies to hygroscopic condensation nuclei? ± What is the collision-coalescence process for forming a raindrop? Why do we say “collision-coalescence” and not just “collision”? Falling Raindrops ± What does “terminal velocity” mean? ± Which falls faster, little droplets or big droplets? ± How does a cloud droplet grow to raindrop size in a cloud when no ice is present? ± Sometimes a falling droplet does not collide with a droplet beneath it. What happens? ± Why doesn’t every pair of droplets that collides
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This note was uploaded on 07/21/2011 for the course MET 1010 taught by Professor Staff during the Fall '08 term at FSU.

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