The Earth's climate is the impact of an adjustment between the sum of the future energy of the sun and the energy transmitted into space. According to NASA's Earth Observatory, approaching solar radiation hits the Earth's environment in the form of unmistakable light, in addition to light and infrared radiation. Ultraviolet (UV) radiation has a higher vitality level than visible light, and infrared (IR) radiation has a lower energy level. Part of the incident solar radiation is ingested by the environment, the seas and the Earth's surface. However, much of it is reflected back into space as low-energy infrared radiation. In order to keep the Earth's temperature stable, the total number of incoming solar radiation must be equal to the total number of incoming solar radiation. Say no to plagiarism. Get a tailor-made essay on “Why violent video games should not be banned”? Get an original essay With the rapid development of the industry, many greenhouse gases such as carbon dioxide (CO2) and methane (CH4), which are released into the atmosphere, increase significantly due to the combustion of fossil fuels. These gases act as a blanket trapping infrared radiation and preventing it from dissipating the atmosphere. The net effect causes a gradual warming of the Earth's atmosphere and surface called the "greenhouse effect." There are several gases called "greenhouse gases" such as carbon dioxide (CO2), chlorofluorocarbons (CFCs) and methane (CH4). They produce a greenhouse effect in the Earth's atmosphere. The most widespread greenhouse gas is CO2. We know that CO¬2 is released into the atmosphere through a natural process. According to the EAP, CO2 accounted for 82% of all U.S. greenhouse gas emissions. Over the past two centuries there has been an increase of 31 percent in CO2 and 150 percent in CH4 (Pakenham, 1998). This is the result of the industry growing over many years by burning coal, oil and gas to produce energy. The industrial revolution also led to the advancement of CFCs, which are widely used in modern applications such as refrigerators, air conditioners, aerosols and many others. The use of these gases was gradually abandoned in the 1990s after it was discovered that “the chemicals eat away at the air”. ozone, an atmospheric layer composed of three oxygen atoms that protect the Earth's surface from ultraviolet rays” (Bradford, 2017). Furthermore, humans also contribute to climate change. Deforestation for fuels (wood and charcoal), industrial products (paper, wood), and the use of tropical forest lands for products like palm oil plantations contribute to the mass deforestation of our world. Forests capture and store carbon dioxide from the atmosphere, and this deforestation releases large amounts of CO2, while reducing the amount of CO2 captured on the planet. 2.2 Effects of “global warming” One of the most obvious and immediate effects of global warming is an increase in average temperatures and extreme weather events. According to the National Oceanic and Atmospheric Administration (NOAA), global temperatures have increased by about 1.4 degrees. Fahrenheit (0.8 degrees Celsius) over the past 100 years and the Earth's surface temperature in 2016 was 1.78 degrees F (0.99 degrees C) warmer than the average for the entire 20th century. Additionally, global warming could also cause weather phenomena.