There are 2 different motions involved in this diagram.The first is the daily motion of the sun as it rises in the east

There are 2 different motions involved in this diagram.The first is the daily motion of the sun as it rises in the eastand then sets in the west at 15°/hr.

Jun

Dec

Since the June path is longer than the December path the sun is in thesky for more hours in the summer than in the winter.

But there is also the annual change in the position of sunrise and sunset.

Jun

Jul

Aug

Sep

Oct

Nov

Dec

In June the sun rises north of east and sets north of west.

JuneSunriseposition

JuneSunsetposition

Jun

Dec

Jan

Feb

Mar

Apr

May

Then, after the winter solstice, the sunrise and sunset positions beginmoving north until it is summer once again.

DecemberSunsetposition

DecemberSunriseposition

And in December it rises south of east and sets south of west.

The Sun follows the middle path on both the Vernal and Autumnal Equinoxes.

On the equinoxes the sun rises due east and sets due west everywhere onEarth and everywhere there are 12 hours of daylight and 12 hours of night.

When the Sun’s path touches this lineit has reached its highest point in the sky for the day.the zenith. That time is called solar noon.

That point is called

The protractor shows the noon altitude of the sun. For example, the altitude of the noon sun in NY on June 21st is about 70⁰.

June

The noon altitude in NY on December 21st is only about 23⁰

Dec

The higher the noon altitude of the Sun, the greater the intensity (strength)of the insolation (sunlight).

June

Dec

That’s why the noon sun is so much more intense in June........

Than in December.

There are two reasons why it’s warmer in summer than in winter:First, the sun is higher in the sky (more intense insolation) in the summer

than in the winter.

Jun

Dec

And second, in the summer the Sun is in the sky for more hours a day whichmeans more time for the Earth to soak up the rays and get warm.

New York city receives more than15 hours of insolation on June 21st.

But only about 9 hoursand15 minutes onDecember 21st That’s a difference

of nearly 6 hours ofdaylight!

Notice that a red pole has been placed in the center of the field. You may beasked to draw the shadow of that pole at noon on any given day.For example, draw the shadow of the pole at noon on March 21st.

First, find the Sun’s path for March 21st. (It’s the one in the middle)Then use a straight edge or ruler to lightly draw a line from Sun’s noonposition, the zenith..... past the tip of the pole, to the ground (dotted line.)

Now draw a line (the shadow) from the base of the pole to the dottedyellow line.Now let’s draw the shadow of the pole as it would appear at noon onDecember 21st.

Find the December 21st path. December 21st has the fewest hours of daylightso it must be the shortest path. Now draw a line from the December zenith, past the tip of the pole, to theground.

Draw the shadow fromthe bottom of thepole to theyellow line.

Notice that the December shadow (red line) is much longer than the Marchshadow (blue line).As the altitude of the Sun increases, the length of a shadow decreases.

In the summer the Sun is here at noon.

In the winter it is here.

On any other day it must besomewhere in between.But on how many days is the Sundirectly overhead, 90°, at noon?

The Sun is never directly overhead anywhere in the United States(except for Hawaii)!

Lastly, let’s look at the relationship between the position of the sunrise inNYS and the location on the Earth where the Sun’s rays are directlyoverhead, 90°.When the Sun rises north of east in NYS as on the summer solstice.......

its direct rays fall on the Tropic of Cancer, 23.5° north.When the Sun rises due east as it does on both equinoxes.....

its direct rays fall on the equator

And when the Sun rises south of east in NYS as on the winter solstice....

its direct rays fall on the Tropic of Capricorn, 23.5° south

What you must understand and know how to do....

For both solstices and both equinoxes.........................

> Know the location of sunrise and sunset> Know the approximate altitude of the Sun at noon.

> Know when the intensity of insolation is least and when it is greatest

> Know the relationship between the altitude of the Sun and shadow length

> Know how to draw the shadow of a pole on a given date> Know where (latitude) the Sun’s direct rays are falling on the Earth> Know when the duration of insolation is greatest and when it is shortest

> Be able to draw the path of the Sun for a given date

> Know that the Sun is never directly overhead anywhere in New York

And most important of all.........

Don’t memorize all this information.........

UNDERSTAND IT!