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Seasonal Change, Solstice and Equinox (redirected from Seasonal Change)

Page history last edited by Robert W. Maloy 1 year, 1 month ago

Animation on Wikimedia Commons by Xofc

The Sun & the ecliptic rotation around the Earth : The green Sun is the one of the vernal equinox (march), it is followed by a summer solstice Sun. Then automn equinox and winter solstice. The ground plane (latitude 50°N) is green, the rotating ecliptic plane is blue. Also represented are the celestial equator, the two tropics and the rotation axis.  Animation on Wikimedia Commons by Xofc

 

In the animation The Sun & the ecliptic rotation around the Earth:

 

The green Sun is the one of the vernal equinox (March)

 

it is followed by a summer solstice Sun.

 

Then Autumnal equinox

 

Then the winter solstice.

 

The ground plane (latitude 50°N) is green, the rotating ecliptic plane is blue.

 

Also represented are the celestial equator, the two tropics and the rotation axis.

 

 

Equinox

 

  • The term, “equinox,” derives from equi-nox (equal-night), and on the equinox, the length of nighttime is nearly equal to the length of daytime,

 

  • Over the previous six months, the sun has been rising in the southeast and setting in the southwest, but on the equinox it rises due east and sets due west, before continuing its northward motion.

 

  • The equinox also marks the start of six months of daylight at the North Pole, and six months of nighttime at the South Pole.

 

Information from Professor Stephen Schneider, University of Massachusetts Amherst

 

 

Learn More at Teaching Latitude, Longitude and Time Zones

 

 


Summer Solstice

  • The first day of summer
  • Longest day of the year
  • This happens when the North Pole is pointing towards the sun
  • Because the North Pole is pointing towards the sun, the Northern Hemisphere is warmed by direct sunlight
  • During summer, the days are long and hot

 

 


Winter Solstice

  • The first day of winter
  • Shortest day of the year
  • This happens with the North Pole is pointing away from the sun
  • Because the North Pole is away from the sun, the Northern Hemisphere does not receive direct sunlight
  • During winter, the days are short and cold

 



Vernal Equinox

  • The first day of spring
  • Equal parts day and night
  • On this day, the North Pole begins leaning towards the sun

 

    • MidPoint is May Day

 

 

 

Autumnal Equinox

  • The first day of fall
  • Equal parts day and night
  • On this day, the North Pole begins leaning away from the sun

 

 



For more information, see The Changing Seasons: A Brief Tutorial

 

Fairbanks Goldpanners Midnight Baseball Game

How Alaskans Cope with Two Months of All-Day-Daylight

 

     Learning Activities

 

Click here for a learning plan about the seasons.


Click here for a learning plan about the seasons.

 

 


  Click here for a youtube video on the changing seasons.

 

 

 

 Need to find a song about the seasons.

 

 

Mayan Calendars                                                                                                                                                                    

            

 

This image shows the Haab calendar (right) interwoven with the Tzolk'in calendar (left). In the Calendar Round, any given combination of a Tzolk’in day with a Haab day will not repeat itself, until 52 periods of 365 days have passed. The Maya believe that when a person turns 52, they attain the special wisdom of an elder.

 

Click here for more images of Mayan Calendars, descriptions of how they were created and videos of

present-day Mayan Calendar keepers.         

This image shows the Mayan Haab calendar interwoven with the Mayan Tzolk'in calendar

 

 


 

 

 

 

 

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