Monday, November 22, 2010

CLIMATE CHANGE


The Earth can undergo climate change in a variety of ways. One major way is by the means of “greenhouse gases”. In Earth’s atmosphere, certain gases (under label of greenhouse gas) trap the solar energy “reradiated” from the earth. This contributes to the warmer temperatures of the climate, and the habitability of the Earth. However, since the late 19th century, when the age of industry and fossil fuels really took off, global temperatures have been slowly increasing. From the late 1800s to today, the increase has been about 1 degree Fahrenheit (1). This is blamed on the excessive amounts of greenhouse gases being emitted by humans. To verify, we need to investigate the various types of greenhouses gases in the atmosphere.

http://www.umich.edu/~gs265/society/gaspie.gif

 

 
http://www.umich.edu/~gs265/society/greenhouse.htm
The “greenhouse effect” is natural in nature. Without it, the Earth would 33 degrees Celsius cooler than it is now (3). That would kill majority of life on Earth, humans included.  The way the greenhouse effect works is similar to a blanket. The Sun sends solar radiation down to Earth. Some of it passes through the atmosphere. This radiation then proceeds to warm the Earth. After warming, radiation is reradiated back towards space. Most of this radiation then escapes Earth, but not all of it. The rest is trapped by the greenhouse gases, adding to the overall global temperature (3). Water vapor is the most abundant greenhouse gas. Think about the Earth, roughly 70% of it is covered with water. A lot of this water gets into the atmosphere and serves as a greenhouse gas. However, water vapor is versatile “gas”. In the atmosphere, it goes through loops. Water vapor blocks the sun’s radiation, turns into clouds, and then cools the atmosphere. It is difficult for scientists to measure accurately. (2) Carbon dioxide makes up the semi-majority of greenhouse gases and second most abundant. It is released into the atmosphere by humans exhaling, burning of fossil fuels, and even deforestation. Methane is another natural greenhouse gas, perhaps more potent. It is released into the atmosphere primarily by cows (passing gas) and the process of plant decay.  It only stays in the atmosphere for 10 years, “but traps 20 times more heat than carbon dioxide (3)”. Nitrous oxide is another gas that is released by human/animal waste. This gas can stay in the atmosphere up to 100 years. Ozone is a natural greenhouse gas by means of absorbing UV light from the sun. Ozone particles in the stratosphere absorb excess amounts of UV-B radiation from the sun. Upon absorbing, said radiation, they produce heat, similar to how a greenhouse gas traps heat (4). Fluorocarbons are more human responsible greenhouse gas. HFCs (hydrofluorocarbons), the substitute for the ozone-killing CFCs, are greenhouse gas material. Instead of killing the ozone layer, they heat up the Earth’s atmosphere (4).

Not all of climate change can be blamed on humans as most people would think. Volcanoes can be a big player in the “climate change picture”. When a volcano erupts, most people would think that just lava comes out. Lava is just a part that comes out, large amounts of gases and dust particles are also thrown into the atmosphere. Dust particles can stay in the air for days to months, depending on where they are in the atmosphere. During this time, these particles can block the sun and produce “cooling effects”. Following the eruption of the volcano “Tambora” in 1815, a severe cooling effect with cold temperatures caused crop failure in North America and Europe (5). Volcanoes that eject sulfur oxide/dioxide can affect the climate even more greatly. This sulfur oxide/dioxide reacts with water in the stratosphere to form droplets of sulfuric acid. Surprisingly, these droplets reflect a great amount of sunlight, producing an even greater cooling effect (5). A volcano can also contribute to global warming by ejecting mass amounts of carbon dioxide into the atmosphere (5).

http://www.bugbog.com/images/galleries/costa-rica-pictures/costa-rica-arenal-volcano.jpg


Works Cited
1.       Global Warming FAQ. NOAA, 20 Aug. 2008. Web. 22 Nov. 2010.
2.       Greenhouse Gases. NOAA, 23 Feb. 2010. Web. 22 Nov. 2010.
3.      3.   Hopwood, Nick, and Jordan Cohen. Greenhouse Gases and Society. University of Michigan. Web. 22 Nov. 2010.
4.    Science: Ozone Basics. NOAA, 20 Mar. 2008. Web. 22 Nov. 2010.
5.  Volcanoes & Climate. Wheeling Jesuit University, 30 Sept. 2010. Web. 22 Nov. 2010.

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LIGHTNING

Lightning strikes all over the world, very numerously in fact. Satellite data suggests there are "3 million lightning flashes worldwide per day". It can happen anywhere there is a storm cloud brewing.(4)









Storm clouds are generally cumulonimbus clouds. These are massive, towering clouds often reaching high in the atmosphere. They usually form when a cold front meets a warm front. The air also has to be moist enough for the clouds to form. Inside the clouds there are strong updrafts. This is the start of how lightning is made. (3)






The exact science how lightning is made is a mystery. There a few theories, but perhaps the most popular one involves ice particles. When a cumulonimbus cloud reaches a precipitation capacity, water is carried up the cloud by the updrafts. Here the water collides with ice particles in the upper portions of the cloud. These collisions supposedly create a charge, which the negative portion going towards the bottom of the cloud and the positive towards the top. The difference in charge becomes too great, and thus, lightning is born. (1)








To summarize, for lightning to exist, there must be a cumulonimbus cloud. Inside the water must collide with enough ice particles to make a great enough charge. If a cumulonimbus cloud produces lightning, then it is classified as a "thunderstorm". (3)














On a side note, lightning ALWAYS exists with thunder. (1)





Technology does exist that detects lightning, but it is hard to predict lightning, for it is random. The detected lighting is almost always CG (cloud-to-ground) Lightning detectors have been in place in the US since the 70s. These antennae detectors are hundreds of kilometers apart and detect the radio-frequency pulses that lightning gives off. The location is where the vectors intersect. Since 1994, this system is one combined network run by Global Atmospherics Inc. These instruments provide lightning strike indicators to provide early storm intelligence and give people an early heads up. (4)











It is estimated that $4-5 billion damages occur each year because of lightning. Money spent to safeguard sensitive equipment from lightning damages is also enormous. Between the years 1979-2008, lightning killed an average of 58 people each year. Lightning can travel through a power line to an electrical appliance, and anyone using that appliance. It can also travel through plumbing pipes and water to a person in contact with either of those, examples primarily being shower and bath. One out of 5 lightning strike victims die, and 70% of the lucky survivors suffer serious long-term after effects. (4)








Lightning also affects the environment around us greatly. Forest fires are generally caused by lightning strikes to a dense group of trees. Power outages can be traced back to lightning hitting a power grid. However, not all the affects of lightning are negative. Lightning maintains the Earth's electricial balance. It returns the negative charges back to the Earth. Lightning also produces o-zone, which is necessary for the Earth's protection against the sun's harmful UV rays. (1)











1) "About Lightning..." http://www.nssl.noaa.gov/. 8 Feb. 2010. Web. 28 Oct. 2010



2) Bellante, Anthony. "How Lightning Is Formed." http://www.helium.com/. Web. 28 Oct. 2010





3) "Cumulonimbus Clouds." University of Illinois. http://www.atmos.uiuc.edu/. 7 Aug. 2010. Web. 28 Oct. 2010





4) Henson, Bob. "Lightning:FAQ." http://www.ucar.edu/ 5 Apr. 2000. Web. 28 Oct. 2010











http://www.maniacworld.com/lightning-strike-in-tree.html



http://www.nssl.noaa.gov/faq/faq_ltg.php/



http://www.helium.com/items/1522307-how-lightning-is-formed



http://www.youtube.com/watch?v=kLJ6oqToKrc&feature=related