6.  How can you explain any differences between your predicted and actual temperatures?
Marks were approximate, and temperature depends on more than elevation, latitude, and precipitation (though those are important factors!).
7.  Kansas City and Springfield have the same average yearly temperature.  Why?
They are similar in all three attributes, and Kansas City's slightly higher elevation has an effect similar to Springfield's slightly higher precipitation.
8.  Denver and Kansas City are located at the same latitude, but Kansas City is warmer.  Why?
Denver is at a much higher elevation, where low air pressure makes the air thinner and less insulating.
9.  Boston and Juneau are located at similar elevations, but they have very different average yearly temperatures.  Why?
Boston is at a much lower latitude (it is closer to the equator), so it receives much more direct sunlight.
10.  	The higher the elevation, the lower the temperature.
	The further north in latitude, the lower the temperature.
	The more water, the lower the temperature.
11.  The interaction of the factors we have learned about is much more complex than we have let on.  Water, for example, doesn’t always lower the temperature of an area.  Large amounts of rainfall tend to lower the average temperature (heat is absorbed as water evaporates), but nearby bodies of water simply help maintain a relatively constant temperature.  While wind itself is caused by differences in temperature and pressure, what other factors influence how air and water vapor move?  What evidence or examples show these factors exist?
Where sunlight strikes (a result of cloudcover, pollution, and other factors) is important.
Other key factors are geographic.
For example, clouds cool as they go higher in the sky, and when clouds try to pass over tall mountains they often lose their water.  This explains the rain shadow we find on the east side of the Rocky Mountains.
If there are no bodies of water, there is no water to evaporate.  This is one of the main reasons deserts can be found all around the world, even where temperatures are not high.
Lastly, humans can have an effect on their weather, including their contributions to pollution, changes to the landscape which make it more or less reflective, and landscape changes which change how water flows and is retained.