The Science
Warning!
This article will contain Science based information!
Seven years ago, when I started to study climate science in earnest, I went to the National Academies of Science, the American Chemistry Society, the American Geophysical Union, the American Association for the Advancement of Science and many more. What I learned then, I will pass on to you.
Science is making a comeback in the climate change debate because people like it. One professor, Michael Ranney, thinks we warm to science if it is put in words everyone can understand. His team’s videos are at, www.howglobalwarming works.org.
Here are three descriptions of our atmosphere’s heating mechanism. The first is by the professor. The second is mine and the third is the scientist’s long version.
Professor Ranney: Earth transforms sunlight’s visible light energy into infrared light energy, which leaves Earth slowly because it is absorbed by greenhouse gases. When people produce greenhouse gases, energy leaves Earth even more slowly––raising Earth’s temperature.
My description: Our sun’s energy (sunlight) passes through the air as if it were not here. When it arrives at the earth’s surface some is reflected, and some is transformed. If the surface is snow, sunlight reflects and heads back to outer space. If it hits asphalt, sunlight is absorbed and transformed into infrared energy. Think of the last time you stepped barefoot on pavement on a summer afternoon. All this infrared energy will also escape to the cold reaches of space. However, infrared energy must contend with carbon dioxide first! The little CO2 molecule absorbs and then re-emits the heat. This delay, by a small molecule in a small (BUT GROWING) percentage of the atmosphere, controls our earth’s temperature.
Here is the longer description
by the scientists: Human activities are changing Earth’s atmosphere and
increasing Earth’s average temperature. What causes these climate changes?
First, let’s understand Earth’s “normal” temperature: When Earth absorbs
sunlight, which is mostly visible light, it heats up. Like the sun, Earth emits
energy––but because it is cooler than the sun, Earth emits lower-energy
infrared wavelengths. Greenhouse gases in the atmosphere (methane, carbon
dioxide, etc.) let visible light pass through, but absorb infrared
light––causing the atmosphere to heat up. The warmer atmosphere emits more
infrared light, which tends to be re-absorbed––perhaps many times––before the
energy eventually returns to space. The extra time this energy hangs around has
helped keep Earth warm enough to support life as we know it. (In contrast, the
moon has no atmosphere, and it is colder than Earth, on average.)
Since the industrial age began around the year 1750, atmospheric carbon dioxide
has increased by 40% and methane has increased by 150%. Such increases cause
extra infrared light absorption, further heating Earth above its typical
temperature range (even as energy from the sun stays basically the same). In
other words, energy that gets to Earth has an even harder time leaving it,
causing Earth’s average temperature to increase–– producing global climate
change.
[In molecular detail, greenhouse gases absorb infrared light because their molecules
can vibrate to produce asymmetric distributions of electric charge, which match
the energy levels of various infrared wavelengths. In contrast, non-greenhouse
gases (such as oxygen and nitrogen–– that is, O2 and N2) don't absorb infrared
light, because they have symmetric charge distributions even when vibrating.]
Summary: (a) Earth absorbs most of the sunlight it receives; (b) Earth then
emits the absorbed light’s energy as infrared light; (c) greenhouse gases
absorb a lot of the infrared light before it can leave our atmosphere; (d)
being absorbed slows the rate at which energy escapes to space; and (e) the
slower passage of energy heats up the atmosphere, water, and ground. By
increasing the amount of greenhouse gases in the atmosphere, humans are
increasing the atmosphere’s absorption of infrared light, thereby warming Earth
and disrupting global climate patterns.
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