Match the Latitude with the data most nearly equal to the data you obtained in the simulation. The data will be for the noon sun's angular height above the horizontal on the four seasonal transition days of the year. (Summer Solstice, Autumn Equinox, Winter Solstice, and Vernal Equinox. Remember that all measurements have small errors so your values might be slightly different but they should not be more than 10% different than those presented hear. If they are you might need to redo this portion of the lab. The answers below represent the angle of the Sun's noon time angle above the horizon at that latitude on that day.

- A. B. C. D.	Summer Solstice - 90 degrees; Autumn Equinox - 66.1 degrees; Winter Solstice - 43.0 degrees; Vernal Equinox - 66.6 degrees
- A. B. C. D.	Summer Solstice - 71.6 degrees; Autumn Equinox - 47.6 degrees; Winter Solstice - 24.8 degrees; Vernal Equinox - 48.5 degrees
- A. B. C. D.	Summer Solstice - 46.9 degrees; Autumn Equinox - 23.3 degrees; Winter Solstice - 0.1 degrees; Vernal Equinox - 23.5 degrees
- A. B. C. D.	Summer Solstice - 23.4 degrees; Autumn Equinox - 0.2 degrees; Winter Solstice - 23.4 degrees; Vernal Equinox - 0.0 degrees

A.	41º N
B.	66.5ºN
C.	23.5° N
D.	90º N