The Earth's Seasons

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Topic 1 – The Earth’s Seasons

1. Seasons of the year. (n.d.). Retrieved December 9, 2011, from National Aeronautics and Space

Administration website: http://www-istp.gsfc.nasa.gov/stargaze/Sseasons.htm

If Earth’s axis were perpendicular to the ecliptic (Earth’s orbital path around the Sun), the Sun’s position in relation to Earth would always be halfway between the North and South Poles; its view from any point on Earth would be the same every day; and every point on Earth, except at the poles, would be in shadow (night) half the time and in sunlight (day) half the time. Because Earth’s axis of rotation is tilted from the perpendicular, Earth experiences seasons. The spring equinox occurs about March 21 and the fall equinox occurs about September 22 and during this time the length of day and night is equal. The summer solstice occurs about June 21 and the winter solstice occurs about December 21. The North Pole is tilted toward the Sun during the summer solstice and faces away from the Sun during the winter solstice (Seasons, n.d.).

2. Astronomical theory of climate change. (n.d.). Retrieved December 9, 2011, from National

Oceanic and Atmospheric Administration website:

http://www.ncdc.noaa.gov/paleo/milankovitch.html

Milutin Milankovitch, a Serbian astronomer, developed an astronomical theory that explains climate change. When the tilt of Earth’s axis changes, the severity of the seasons changes; a greater degree of tilt means warmer summers and cooler winters, while a decrease in the tilt means coolers summers and warmer winters. Because Earth wobbles in orbit, the tilt can range from 22 degrees to 25 degrees on a 41,000-year cycle. Currently, the tilt is at 23.5 degrees. Other...

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... for marine life. During an El Niño event, westerly winds at the western end of the basin permit warm water to flow eastward and trade winds weaken. The storm zone and atmospheric convection move with the warm water resulting in heavy rainfall and flooding along coastal areas of western South America. The thermocline (the boundary layer between the warm surface water and the deeper, colder water) deepens and the cold water isn’t pushed up, which deprives marine life of necessary nutrients. During a La Niña event, trade winds grow stronger and the warm pool shrinks, which results in a colder, drier climate off the coast of America. Atmospheric convection is restricted to the western end of the basin and abundant rain falls over Indonesia. Cold waters along the west coast of South America surge upward and nutrients are plentiful for marine life (El Niño, n.d.).

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