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reasons for the seasons

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AB
autumnal equinoxalways in interval September 20-22
vernal equinoxalways in interval March 20-22
winter solsticealways in interval December 20-22
summer solsticealways in interval June 20-22
23.5 degreesangle between earth's axis & its path of orbit around the sun
elipticalan orbit that is not a perfect circle
summer in the Northern hemispherebegins on longest day of year & ends on day w/ about 12 hours between sunrise & sunset
winter in the Northern hemispherebegins on shortest day of year & ends on day w/ about 12 hours between sunrise & sunset
winter at North pole of earthdark 24 hours/day
Summer at North pole of earthlight 24 hours/day
distance between earth and sun, on average93,000,000 miles or 1 astronomical unit (1 AU)
days of the year at the equator when the sun is directly overhead (90 degrees altitude) at its zenithautumnal equinox AND vernal equinox
at equator, azimuth of sunrise on autumnal equinox or vernal equinoxdue east, 90 degrees
at equator, azimuth of sunset of autumnal equinox and spring equinoxdue west, 270 degrees
convection currents over water that is warmest over equator, then cools gradually at increasingly N or S latitudesmovement of winds away from the equator & control of moisture content at different latitudes


AP biology, biology, biochemistry, and chemistry teacher
Mayfield High School
Mayfield Village, OH

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