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The Earth has been in an ice age for quite some time, which is interrupted
by periods of "interglaciation" (warm climate) about every 100,000 years, when mean global temperatures rise 10 to 12 degrees
Celcius.

The blue line in the graph above is a reconstruction of global temperatures
for the past 450,000 years taken from ice cores from the Vostock glacier in Antarctica. The green line in the graph above
shows how closely changes in carbon dioxide and temperature correlate. But as you can see, the man made increase in atmospheric
carbon dioxide (in red) nearly sky-rockets off this chart, but the temperature does not follow.
Also, some have tried to say that CO2 has caused temperature changes
during this time; not true. "... new high-resolution studies show that at times of cold to warm transitions, temperature
changes come first, leading CO2 changes by several centuries (Mudelsee, 2001; Clark, 2003; Vakulenko et al., 2004). If so,
the CO2 levels would be response to, and not a cause of, the change in temperature (climate). CO2 may then serve as a temperature
amplifier, but not as the climate driver." (C6)
It is generally understood that periods of glaciation and interglaciation
are caused by changes in the Earth's orbit around the sun, not by changes in atmospheric CO2 as some have recently tried to
suggest.

The graphics above represent the changes in the Earth's orbit around
the sun. There are also changes in the Earth's angle and wobble as it moves through space that contribute to major climate
changes. Taken together they are known as the "Milankovitch Cycles." As the Earth goes farther away from the sun, or as the
angle of the Earth changes, climate changes.
The Spectrum
Photons are the basic unit of light, they are particles that have no
charge or mass. They are also called electromagnetic radiation. The photon is always the same thing, but oscillates at different
speeds. The spectrum is how light is organized from the fastest oscillation to the slowest. There are six types of light in
the spectrum; radio waves, infrared, visible light, UV light, X-ray, and gamma rays. Each part of the spectrum has its own
frequency (number of oscillations in a second) and wavelength (the distance in which a photon travels at the speed of light
in one oscillation). The photons with the highest frequency and the shortest wavelengths have very high energy (the gamma
rays). The low frequency photon with the longest wavelength has low energy (radio waves).
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