Definitions
- What is insolation?
- What is meant by atmospheric pathlength?
- What is the tilt of the earth's axis?
- What is meant by parallelism?
- What is the circle of illumination?
- What is the sun angle measuring?
- What is the definition of declination?
- What is an equinox?
- What is a solstice?
Content
- What are the 3 main factors affecting the amount of insolation received at a particular place?
- Of these 3 factors, which 2 are the most important?
- How does the amount of insolation received at a particular place affect temperature?
- What are the motions of the earth, and how do these motions affect the amount of insolation received at a particular place?
- What is the declination of the sun on the March equinox, the June solstice, the September equinox and the December solstice?
- Does your location affect the declination? If not, what determines the declination?
- Why is the declination important with regards to the amount of insolation received at a particular place?
- What affect does sun angle have on the amount of insolation received at a particular place?
- At any given location (e.g. Stevens Point, WI or Christchurch, NZ), how does the sun angle change throughout the day and throughout the year? Why?
- On any given date (e.g. the March equinox), how does the sun angle change as latitude changes? Why?
- At noon, is the sun angle in Stevens Point higher in January or July? Why?
- What affect does day length (hours of sunlight) have on the amount of insolation received at a particular place?
- At any given location (e.g. Stevens Point, WI or Christchurch, NZ), how does day length (hours of sunlight) change throughout the year? Why?
- On any given date (e.g. the March equinox or the June solstice), how does the day length change as latitude changes? Why?
- What affect does atmospheric thickness have on the amount of insolation received at a particular place?
- At any given location (e.g. Stevens Point), at what times of the day does sunlight have the greatest pathlength to reach the surface?
- On any given date (e.g. the March equinox or the June solstice), at what latitude does sunlight have the greatest pathlength to reach the surface?
Karen A. Lemke: klemke@uwsp.edu
Last revised January 19, 2007